ILLINOIS  STATE  GEOLOGICAL  SURVEY 


3  3051  00000  2836 


jWW 


fUG 


O*** 


n.***** 


\    ^ 


Digitized  by  the  Internet  Archive 

in  2012  with  funding  from 

University  of  Illinois  Urbana-Champaign 


http://archive.org/details/oilfieldsofcrawf22blat 


ILjijllNV^lO      Olrt  ir>      VJ  F^KJ  l.UUH_  f\  .L,      OL    x» 


R  IX  E  RXE  R  XI  E      R  XIV  W  RXIIIW R 


R  XI   W  R  X  W 


MANZ-CHICAGO 


Map  showing  the  oil  and  gas  fields  of  Southeastern    Illinois    and    the    quadrangles    covered    by 

this    report. 


STATE   OF  ILLINOIS 
STATE   GEOLOGICAL  SURVEY 

FRANK   W.  DeWOLF,  Director 


BULLETIN  No.  22 


THE  OIL  FIELDS 


OF 


Crawford  and  Lawrence  Counties 


BY 


RAYMOND  S.  BLATCHLEY 


URBANA 

University  of  Illinois 
19  13 


Springfield,  III. 
Illinois  Statb  Journal  Co..,  Stat*  Printi 
19  13 


STATE  GEOLOGICAL  COMMISSION. 


Edward  F.  Dunne,  Chairman, 
Governor  of  Illinois. 

Thomas  C.  Chambeblin,  Vice-Chairman. 

Edmund  J.  James,  Secretary, 
President  of  the  University  of  Illinois. 


Feank  W.  DeWolf,  Director. 
Feed  H.  Kay,  Ass't.  State  Geologist. 


CONTENTS. 


Chapter  I. 

Historical,  Theoretical,  and  Geological  Aspects  of  the  Illinois  Fields. 

Page. 

Object  of  report 11 

Methods  of  study 11 

Acknowledgments 12 

Historical  review  of  oil  developments  in  Illinois 12 

Original  and  accumulation  of  oil 16 

Origin  of  oil 16 

The  inorganic  theory 16 

The  organic  theory 17 

Circulation  and  accumulation  of  oil 18 

General  considerations 18 

The  porous  stratum 21 

Impervious  cover 22 

Geological  structure 22 

Water  saturation 24 

General  geology  of  Illinois  relating  to  oil  and  gas 24 

Introduction 24 

Stratigraphy 25 

Areal  extent  of  the  formations  and  oil  sands 27 

Structure 32 

Stratigraphy  of  Crawford  and  Lawrence  counties 32 

General  statement 32 

Crawford  county 32 

Logs 33 

Stratigraphy 52 

Pleistocene 52 

Pennsylvanian 53 

McLeansboro  formation 53 

Carbondale  formation 53 

Pottsville  formation 54 

Lawrence  county 54 

Logs 54 

Stratigraphy 82 

Pleistocene 82 

Pennsylvanian 82 

McLeansboro  and  Carbondale  formations 82 

Pottsville  formation 82 

Mississippian 83 

Birdsville  and  Tribune  formations  (upper  portion  of  Chester  group) 83 

Ste.  Genevieve  formation 84 

St.  Louis  formation 85 

Chapter  II. 

General  Description  of  Features  of  the  Main  Oil  Fields. 

Introduction 86 

Field  work 86 

Topographic  surveys  of  the  area 86 

Levels  in  the  oil  fields 87 

Hardinville  quadrangle 87 

Sumner  quadrangle 89 


Contents — Continued. 

Page. 
Field  work— Concluded. 

Geographic  positions  of  quadrangles 91 

Hardinville  quadrangle 91 

Sumner  quadrangle 93 

Vincennes  quadrangle 93 

Elevations  of  oil  wells 94 

Collection  of  well  records 94 

Geological  aspects 95 

General  statement 95 

Local  names  of  sands 95 

Correlation  of  sands 95 

Altitudes  of  sands 95 

Tables  of  well  data 96 

Contour  maps 96 

Cross-sections . : 96 

Chapter  III. 
Detailed  Geology  of  the   Crawford    County  Field. 

General  features  of  the  oil  field 97 

Detailed  structure  of  the  district 99 

Relations  of  structure  to  oil  and  gas 100 

Relations  of  salt  water  to  structure 103 

Conclusion 104 

Chapter  IV. 
Detailed   Geology   of  the   Lawrence    County    Field. 

General  features  of  the  oil  field 105 

Detailed  structure  of  the  district 106 

The  "shallow"  sand 1 106 

Bridgeport  sand 106 

Buchanan  sand 107 

Detailed  structure 107 

"Gas"  sand % 108 

Detailed  structure 109 

Kirkwood  sand 109 

Detailed  structure 110 

Tracey  sand Ill 

Detailed  structure 112 

McCloskey  sand 112 

Detailed  structure 113 

Cross-sections 114 

General  statement 114 

Cross-section  A-A 114 

Logs 115 

Cross-section  B-B 123 

Logs 123 

Cross-section  C-C 125 

Logs 125 

Cross-section  D-D 130 

Logs 130 

Relations  of  structure  to  oil  and  gas 135 

Oil 135 

Petty  township 136 

Bridgeport  township 137 

Lawrence  township 137 

Dennison  township ' 137 

Gas 138 

Petty  township 139 

Bridgeport  township 139 

Lawrence  township 140 

Dennison  township 140 


Contents — Concluded. 

Page. 
Relations  of  structure  to  salt  water 14° 

140 

Petty  township 

Bridgeport  township 14° 

Lawrence  township 14° 

Dennison  township 

Chapter  V. 
General  Summary  of  Geological  Conditions  in  Crawford  and  Lawrence  Counties. 

General  statement 

General  structure  of  the  region  of  the  LaSalle  anticline 142 

Detailed  features  of  the  fields '- 

Prospective  pools : 

Chapter  VI. 

Economic  Features  of  the  Illinois  Fields. 

145 
Introduction " 

Development  of  oil  properties 

Forenote - : 14Q 

Leasing * 

Choosing  a  well-site 

Drilling JJ 

Shooting  a  well ^ 

Lease  equipment 15 

Cleaning  out  and  tubing  the  well 157 

Tanks \f 

Loading  racks 

Power  and  boiler  houses •• 158 

Pull-rods  and  pumping  discs 159 

Pumping  jacks j^9 

Removal  of  salt  water  and  steaming  oil 159 

The  approximate  cost  of  oil  wells 160 

The  cost  of  operating  a  lease 161 

Investmentsin  oil  properties • j*^ 

Buying,  transporting,  and  storing  oil 

Buying  oil ^ 

Transport'ng  the  oil 

Storing  the  oil jjjjj 

Independent  oil  companies 

Prices  and  pipe-line  runs  of  Illinois  oil 167 

Prices  of  Illinois  oil 167 

Pine-line  runs  and  stocks  of  Illinois  oil 169 

1  fiQ 

Summary  tables 

Natural  gas  in  Illinois jjjj 

Tables  of  well  data  (appendix) 


ILLUSTRATIONS. 


Plate.  Page . 
1A.    Map  showing  the  oil  and  gas  fields  of  Southeastern  Illinois  and  the  quadrangles  cov- 
ered by  this  report Frontispiece 

IB.    Section  across  southern  Illinois  through,  Monroe,  Clinton  and  Lawrence  counties 32 

II.    Columnar  sections  in  Crawford  county 34 

III  A.    Columnar  sections  in  Lawrence  county 54 

IIIB .    Diagram  showing  correlation  of  the  Robinson  and  Bridgeport  sands 84 

IV.    Base  map  of  the  Crawford  county  oil  field— Southern  half— showing  developments  to 

Jan.  1, 1909 Pocket 

V.    Crawford  county  oil  field  showing  structure  contours  on  top  of  the  Robinson  sand — 

first  lens Pocket 

VI.    Base  map  of  the  Lawrence  county  oil  field  showing  development  to  July  1,  1911 Pocket 

VII.    Lawrence  county  oil  field  showing  structure  contours  on  top  of  the  Buchanan  sand .  Pocket 

VIII.    Lawrence  county  oil  field  showing  structure  contours  on  top  of  the  "  Gas  "  sand Pocket 

IX.    Lawrence  county  oil  field  showing  structure  contours  on  top  of  the  Kirkwood  sand  .  Pocket 

X.    Lawrence  county  oil  field  showing  structure  contours  on  top  of  the  Tracey  sand Pocket 

XL    Lawrence  county  oil  field  showing  structure  contours  on  top  of  the  McClosky  sand. .  Pocket 
XII.    A-A  longitudinal  section,  Lawrence  county,  along  the  crest  of  the  LaSalle  anticline 

and  through  the  center  of  the  field 116 

XIII.  B-B  cross-section,  Lawrence  county,  across  the  northern  end  of  the  oil  field 124 

XIV.  C-C  cross-section,  Lawrence  county,  across  the  structural  dome  in  Petty  township. .  126 

XV.  D-D  cross-section,  Lawrence  county,  across  the  southern  end  of  the  oil  field 132 

XVI.  The  standard  derrick 146 

XVII.    The  steel  derrick 148 

XVIII.    A—  A  nitroglycerine  plant 150 

B    A  storage  magazine  for  nitroglycerine 150 

XIX.    A— Oil  tanks  under  shed 152 

B— A  pumping  disc 152 

XX.    A—  A  modern  tank-car  loading  rack 154 

JS— An  early  tank-car  loading  rack 154 

XXI.    A—  A  power  or  pumping  house 156 

B— A  boiler  house 156 

XXII.    A—  The  standard  pumping  jack 158 

B— The  steel  pumping  jack 158 

XXIII.  A—  A  third  type  of  pumping  jacks 160 

B— A  town  lot  well  in  Bridgeport,  111 160 

XXIV.  A— A  waste  pit  for  burning  waste  oil 162 

B— The  effect  of  fire  from  waste  oil  on  streams 162 

XXV.    A—  The  Ohio  Oil  Company's  pumping  station,  Stoy,  111 164 

B — The  Tidewater  Pipe  Line  Company's  pumping  station,  Stoy,  111 164 

XXVI.  The  Ohio  Oil  Company's  pumping  station,  Bridgeport,  111 166 

XXVII.  A—  A  portion  of  the  Ohio  Oil  Company's  tank  farm,  Stoy,  111 168 

B— A  cleaning  rig 168 

XXVIII     A  35,000  bbl.,  tank  fire '. 170 

XXIX.    The  tank  after  the  fire 172 

XXX.    A  supply  yard  in  Bridgeport 174 

XXXI.    A—  A  gas  well 176 

B— A  gas  well  with  water  retainer 176 


LETTER  OF  TRANSMITTAL. 


State  Geological  Survey, 
University  oe  Illinois,  January  30,  1913. 

Governor  E.   F.   Dunne,   Chairman,   and  Members   of   the    Geological 

Commission  ; 

gentlemen — I  submit  herewith  a  report  on  the  oil  fields  of  Crawford 
and  Lawrence  counties,  Illinois,  and  recommend  that  it  be  published  as 
Bulletin  No.  22. 

The  author,  Mr.  Eaymond  S.  Blatchley,  has  been  on  the  staff  of  the 
survey  since  1908  and  has  devoted  a  large  part  of  three  years  to  the 
studies  presented  here. 

The  colored  maps  which  accompany  the  report  present  information 
of  great  commercial  value  in  locating  future  wells  in  the  district.  The 
kindness  of  property  owners  and  oil  operators  who  have  contributed  in- 
formation freely  to  the  survey  is  hereby  acknowledged,,  and  confidence  is 
expressed  that  they  will  find  the  report  almost  invaluable. 

Very  respectfully, 

Frank  W.  DeWolf, 

Director. 


BLATCHLEY]  OBJECT    OF    REPORT.  11 


THE    OIL  FIELDS   OF   CRAWFORD    AND   LAW- 
RENCE   COUNTIES,  ILLINOIS. 

By  Raymond   S.   Blatchley. 


CHAPTER  I. 

Historical,  Theoretical,  and  Geological  Aspects  of  the  Illinois  Fields 


OBJECT  OF  EEPOET. 

This  report  presents  the  results  of  a  study  of  the  geologic  conditions 
in  the  southern  half  of  the  eastern  Illinois  oil  fields.  The  specific  area 
of  investigation  lies  in  the  southern  half  of  Crawford  and  the  northern 
portion  of  Lawrence  counties,  in  portions  of  the  Hardinville,  Sumner, 
and  Vincennes  quadrangles  (See  Plate  IA.)  The  object  is  to  discuss  the 
control  of  the  accumulation  of  oil  and  gas  in  these  fields  and  to  present 
facts  which  further  confirm  the  anticlinal  or  structural  theory  for  the 
concentration  of  oil  and  gas  in  raised  formations.  It  is  also  possible 
that  additional  proof  is  added  to  support  the  theory  of  the  origin  of  oil 
from  organic  remains  buried  in  limestone  and  shales.  The  report  also 
discusses  the  stratigraphy  and  describes  the  commercial  features  peculiar 
to  this  territory,  including  production,  costs,  methods  of  transportation 
and  storage,  field  operations,  leasing,  etc.  It  is  desired  to  preserve  in 
printed  form  all  available  records  of  the  territory,  particularly  for  use 
in  future  stratigraphic  and  structural  studies  and  for  reference  by  the 
operators. 

METHODS  OF  STUDY. 

The  method  of  study  was  to  map  by  means  of  contour  lines,  or  lines 
through  points  of  equal  altitude,  the  geologic  structure  of  the  producing 
sands.  The  contours  were  made  upon  the  positive  altitudes  of  the  sands 
above  a  datum  plane  1,500  feet  below  mean  sea  level.  These  maps  show 
the  oil  sand  as  if  everything  above  it  had  been  removed.  The  undula- 
tions, slopes,  basins,  etc.,  are  clearly  defined.  In  this  way  the  oil,  gas, 
and  water  relations  to  the  structure  are  studied.  In  addition  to  the  con- 
tour maps  cross-sections  were  made  along  the  crest  of  the  anticline  and 
crosswise  to  it.     These  graphic   sections  are  intended  merely  to  make 


12  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

clearer  the  contour  maps.  The  records  along  the  selected  lines  are  plotted 
on  a  uniform  scale  and  are  placed  in  their  proper  positions  along  the 
section,  with  regard  both  to  the  elevation  of  the  wells  above  sea  level  and 
to  their  linear  distance  from  one  another.  The  points  at  which  the  cross- 
section  lines  cut  the  contours  are  measured  and  marked  on  the  section. 
AIL  points  representing  a  particular  horizon  are  connected.  Thus,  a 
mechanical  means  of  ascertaining  structural  features  was  developed  and 
significant  facts  were  revealed. 

ACKNOWLEDGMENTS. 

The  taking  of  elevations  and  logs  of  the  wells  within  the  portion  of 
the  oil  fields  covered  by  this  report  began  in  the  summer  of  1908.  The 
writer  was  assisted  in  this  work  by  Douglas  Wright  in  the  Crawford 
county  portion  of  the  Hardinville  quadrangle  and  by  J.  C.  Jones  in 
the  Lawrence  county  division.  The  leveling  in  the  Sumner  and  Vin- 
cennes  quadrangles  was  completed  the  following  summer  with  the  assis- 
tance of  W.  E.  Deuchler,  levelman,  and  Douglas  Wright  and  H.  H. 
Johnson,  rodmen.  A  final  review  of  the  Lawrence  county  fields  was 
made  in  1911  with  the  assistance  of  D.  G.  Thompson.  The  report  would 
not  have  been  possible  except  for  the  hearty  cooperation  of  all  operators 
who  furnished  well  records,  maps,  and  other  information.  Much  help 
was  given  in  the  stratigraphic  studies  by  Dr.  J.  A.  Udden  who  made  an 
intimate  examination  of  well  samples  from  eleven  wells  within  the  in- 
vestigated area.  Special  thanks  are  due  the  officials  of  the  Ohio  Oil 
Company,  Marshall,  111.,  for  samples  from  a  number  of  wells  in  the 
region.  These  were  saved  at  much  trouble  and  expense.  Dr.  Stuart 
Weller  of  the  University  of  Chicago  gave  helpful  consultation  relative 
to  the  stratigraphy  of  the  Mississippian  rocks.  To  all  of  these  indi- 
viduals the  writer  expresses  his  appreciation  and  thanks. 

HISTORICAL  REVIEW  OF  OIL  DEVELOPMENTS  IN 
ILLINOIS. 

In  the  main  fields  of  Illinois,  exclusive  of  producing  areas  elsewhere, 
there  have  been  drilled,  during  the  past  seven  years,  over  20,000  wells 
in  a  producing  territory  which  covers  about  250  square  miles.  The  fol- 
lowing notes  sketch  the  history  of  drilling  from  the  earliest  days: 

In  the  earlier  part  of  the  "sixties"  the  first  oil  excitement  spread  over 
the  eastern  United  States  and  extended  westward  to  Illinois.  In  1865 
the  first  wild-catting  took  place  in  Clark  county  about  8  miles  north  of 
Casey,  in  Parker  township.  Here,  several  holes  were  put  down  in 
attempts  to  locate  oil  and  gas  but  the  work  was  abandoned.  The  small 
amount  of  oil  found  in  the  wells  perhaps  would  have  been  greater  had 
proper  casing  been  used.  This  would  have  shut  off  the  salt  water,  which, 
as  a  matter  of  fact,  probably  drowned  out  the  oil  and  prevented  an  earlier 
discovery  of  the  present  immense  field. 

About  this  time,  oil  and  gas  were  found  accidentally  in  Montgomery 
county,  near  Litchfield.  Coal  prospecting  from  the  floor  of  one  of  the 
mines  led  to  deeper  drilling  and  the  discovery  of  a  strong  flow  of  salt 
water  which  threatened  for  a  time  to  flood  the  mine.    Another  coal  pros- 


blatchley]  HISTORICAL   REVIEW.  13 

pect  near  the  mine  discovered  a  small  quantity  of  oil  and  gas.  The  oil 
and  water  from  this  drill  hole  leaked  into  a  sump  in  the  mine,  where 
for  many  years  oil  was  skimmed  from  the  top  of  the  water  and  utilized. 

During  the  "eighties,"  when  new  prospecting  was  taking  place  at 
various  points  in  Illinois,  the  previous  finding  of  oil  at  Litchfield  led  to 
renewed  drilling  which  brought  in  several  gas  wells  in  that  vicinity.  In 
1882  a  well  was  drilled  about  2  miles  south  of  Litchfield,  which  was 
reported  to  show  about  400  pounds  gas  pressure.  This  well  was  appar- 
ently first  drilled  to  580  feet  without  success.  Two  years  later  it  was 
drilled  200  feet  deeper,  where  water-bearing  sand  was  tapped.  The  gas 
was  secured  at  640  feet  and  had  exceptional  pressure.  The  flow  of  salt 
water,  however,  was  too  strong  to  be  plugged  successfully  and,  conse- 
quently, drowned  out  the  gas.  In  1886  a  number  of  wells  that  yielded 
both  gas  and  oil  were  drilled  in  the  vicinity  of  Litchfield,  to  an  average 
depth  of  about  650  feet.  In  all,  between  the  years  of  1882  and  1889, 
about  thirty  wells  were  drilled.1  The  majority  of  them  were  of  short 
life  but  five  or  six  produced  a  small  amount  of  oil  up  to  the  year  1903. 
All  are  abandoned  at  the  present  time.  , 

Gas  was  discovered  in  Pike  county  in  1886  while  drilling  for  water  in 
the  N.  W.  %  S.  E.  %  section  1,  berry  township.  It  was  found  at  a 
depth  of  186  feet.2  This  destroyed  chances  of  a  good  water  supply  so 
a  second  well  was  drilled  on  the  same  farm  a  short  while  afterwards. 
Gas  was  secured  in  this  well  at  the  lesser  depth  of  168  feet.  Both 
wells  were  abandoned  because  of  lack  of  facilities  for  taking  care  of  the 
gas.  Drilling  was  then  suspended  in  this  part  of  the  State  for  15  years, 
or  until  1905.  In  that  year  Mr.  William  Irick  drilled  a  well  for  water 
on  his  farm  and,  as  in  the  previous  cases,  met  a  strong  flow  of  gas.  He, 
however,  piped  it  to  his  house  for  domestic  use.  /  There  immediately 
followed  a  development  of  this  area,  which,  in  a  little  over  a  year, 
brought  in  over  thirty  wells.  All  but  six  of  these  produced  gas,  but  no 
oil  was  found.  The  gas  horizons  are  between  75  and  350  feet  below  the 
surface.  The  field  at  the  present  time  covers  an  area  about  10  miles 
long  and  4  miles  wide.  The  gas  accumulation  is  governed  by  a  small 
fold  in  the  Niagara  limestone. 

Similar  prospecting  took  place  in  1888  near  Sparta  in  Eandolph 
county.  Home  capital  was  enlisted  and  a  well  that  yielded  a  good  pres- 
sure of  gas3  was  drilled  to  a  depth  of  850  feet.  This  encouraged  further 
drilling  and  up  to  the  year  1894,  22  wells  were  put  down.  Of  these, 
over  twelve  yielded  gas,  and  four  of  them  had  initial  pressures  between 
150  and  250  pounds  to  the  square  inch.  The  average  life  of  the  wells 
was  about  seven  years. 

The  next  recorded  wild-catting  took  place  in  1900,  and  indirectly  re- 
sulted in  the  discovery  of  the  main  oil  field.  A  company  styled  the 
Crawford  County  Oil,  Gas  and  Coal  Company  drilled  a  well  in  the  S.  E. 
y^  section  35,  Eobinson  township,  Crawford  county.4  The  well  reached 
a  depth  of  820  feet  where  it  was  abandoned  because  of  the  caving  of 
the  strata  and  the  tapping  of  a  strong  vein  of  salt  water.  The  same 
company  shifted  operations  in  the  following  year,  1901,  to  the  D.   C. 

i  Mineral  Resources  of  the  United  States  for  1889,  p.  353. 

2  Savage,  T.  E.,  Pike  County  gas  field:    Bull.  111.  Cxeol.  Survey  No.  2, 1906,  p.  83. 

3  Report  Illinois  Board  World's  Fair  Commissioners,  1893,  p.  183. 

*  Blatchley,  W.  S.,  Oil  Developments  in  Illinois  to  K04:     Bull.  111.  Geol.  Survey  No.  2, 1906,  p.  14. 


14  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 

Jones  farm,  in  the  southwest  quarter  of  section  22  of  the  same  town- 
ship. A  well  drilled  here  to  a  depth  of  1,040  feet  secured  a  small 
amount  of  gas.  Thus,  the  efforts  of  the  company  to  locate  "fuel"  were 
rewarded  slightly  and  with  further  hope,  they  drilled  to  1,190  feet.  At 
this  point  they  met  a  strong  vein  of  salt  water  and  abandoned  the  well. 
The  company  attempted  other  wells  on  the  same  farm  in  the  years 
1901,  1902  and  1903,  but,  in  each  case,  lost  their  tools.  The  sixth 
attempt  was  rewarded,  in  1904,  by  the  finding  of  small  amounts  of  oil 
and  gas  between  900  and  1,200  feet.  The  bore  was  carried  to  1,330 
feet  but  was  abandoned.  It  was  but  eighteen  months  after  this  that 
the  main  productive  field  was  opened  up  within  a  few  miles  of  this  area. 

The  suggestion  of  an  oil  field  in  the  vicinity  of  Casey  prompted  by  the 
earlier  prospecting  of  the  "sixties,"  led  Col.  L.  D.  Carter  of  Oakland, 
111.,  to  secure  the  services  of  J.  J.  Hoblitzel  &  Son,  of  Pittsburgh, 
Pa.,  in  re-drilling  this  area.  A  large  block  of  lease  was  gathered  up,  and 
early  in  the  spring  of  1904  a  well  was  started  on  the  Young  farm  near 
Oilfield.  This  well  produced  a  good  pressure  of  gas  and  some  oil.  The 
gas  was  cased  off  and  used  for  field  operations  but  the  oil  yield  was  in- 
significant and  was  discarded.  A  second  well  was  completed  in  the  same 
year  on  the  J.  S.  Phillips  farm  in  the  northeast  quarter  of  section  18, 
Parker  township.  It  produced  35  barrels  of  oil.  Other  wells  were 
started  in  the  same  year  in  this  vicinity  and  in  1905  about  100  square 
miles  of  territory  was  being  drilled.  Of  this  about  60  square  miles  were 
eventually  found  productive.  These  fields  are  called  the  "shallow"  area 
because  the  oil  comes  from  a  depth  of  between  400  and  600  feet.  Drilling 
was  active  until  1909,  when  the  boundaries  of  the  productive  territory 
for  this  section  of  the  oil  fields  were  pretty  well  established.  In  1909 
there  was  a  decreasing  development  and  at  the  present  time  it  has  prac- 
tically ceased.  A  great  many  of  the  original  wells  are  yielding  so  poorly 
that  they  are  rapidly  being  plugged  and  abandoned. 

Added  vigor  was  given  to  the  development  of  the  eastern  Illinois 
fields  on  February  6,  1906,  when  D.  T.  Finley,  of  Pittsburgh,  drilled  a 
well  on  the  J.  W.  Shire  farm  in  the  northwest  quarter  of  section  15, 
Oblong  township,  Crawford  county.  The  oil  was  obtained  at  890  feet, 
and  the  initial  production  was  250  barrels  per  day.  This  well  opened 
up  the  Robinson  pool,  which  is  the  largest  in  the  oil  area  and  covers,  in 
all,  about  110  square  miles  of  productive  territory.  The  oil  is  found 
in  sands  ranging  from  750  to  1,000  feet  in  depth.  There  is  one  general 
sand  made  up  of  three  or  more  generally  parallel  lenses.  There  arer 
however,  small  areas  where  only  two  or  even  one  lens  are  noted. 

The  year  1907  brought  an  extension  of  development  in  a  small 
isolated  pool  about  three  miles  to  the  southeast  of  the  large  Robinson 
pool.  The  new  pool  was  known  first  as  the  Honey  Creek  district  and 
originally  covered  but  six  or  seven  square  miles.  It  has  later  been  asso- 
ciated with  the  Flat  Rock  district  to  the  east  and  the  two  are  now 
joined,  so  as  to  comprise  about  25  square  miles  of  area.  To  the  north 
of  the  Flat  Rock  area  the  small  Duncanville  pool  was  developed.  The 
area  covered  is  between  two  and  three  square  miles.  The  oil  is  from 
about  the  same  horizon  as  that  of  the  Honey  creek,  Flat  Rock,  and 
Robinson  sands  but  has  a  much  lower  gravity.  It  is  used  almost  ex- 
clusively for  fuel. 


BLATCHLEY]  HISTORICAL    REVIEW.  15 

The  Lawrence  county  field  began  to  be  developed  actively  in  1907- 
1908.  It  has  been  the  most  promising,  in  that  seven  sands  are  attracting 
the  attention  of  operators.  The  sands  occur  between  depths  of  800  and 
1,900  feet  and  are  known  as  follows : 

1,  2  and  3.     Bridgeport,  upper  lens,  middle  lens  and  lower  lens. 

4.  Buchanan. 

5.  Kirkwood. 

6.  Tracey. 

7.  McClosky. 

Within  this  area,  which  covers  about  40  square  miles,  there  has  been 
developed  a  larger  per  cent  of  big  wells  than  in  all  other  pools  in 
Illinois  combined. 

After  the  Clark  county  fields  was  brought  in  miscellaneous  drilling 
was  stimulated  throughout  the  State.  A  second  attempt  was  made  to 
discover  oil  in  the  vicinity  of  Sparta,  111.  by  J.  J.  Hoblitzell  &  Son, 
who  began  drilling  in  1906.  As  a  result  of  this  work,  two  or  three  wells 
that  produced  oil  in  small  quantity  were  completed  in  the  following 
year.  In  1908  a  total  of  sixteen  wells  had  been  drilled,  but  of  these 
only  six  or  seven  yielded  oil.  The  amounts  were  small,  except  in  the 
case  of  two  wells,  one  on  the  Foster  farm  that  yielded  about  twenty 
barrels  of  oil  per  day,  and  one  on  the  Mcllroy  farm  that  had  an  initial 
production  of  about  100  barrels.  All  the  wells  have  since  declined  and 
the  field  is  now  abandoned. 

In  1906  an  attempt  was  made  to  locate  oil  at  Tolono  in  Champaign 
county.  The  drilling  revealed  oil,  but  only  in  slight  quantity.  Ap- 
parently it  was  the  intention  to  prospect  the  La  Salle  anticline  which 
gives  rise  to  the  production  area  to  the  southeast. 

Early  in  the  year  1908,  oil  was  reported  as  seeping  through  a  fault 
into  a  coal  mine  near  Centralia,  Marion  county.  The  attention  of  oil 
operators  was  excited  and  several  shallow  wells  were  drilled.  These 
yielded  small  amounts  of  oil,  but  were  of  slight  commercial  value.  Wild- 
catting  was  prompted  in  the  winter  of  1909  in  the  vicinity  of  Sandoval, 
five  miles  north  of  the  Centralia  shallow  wells.  Late  in  March,  a  deep 
well,  which  yielded  about  thirty  barrels  per  day,  was  completed  upon  the 
Stein  farm,  one  mile  north  of  Sandoval.  A  second  well  was  finished  in 
July  on  the  Benoist  farm,  adjoining  the  Stein  land.  This  well  proved 
to  be  a  valuable  producer  of  both  oil  and  gas.  Its  success  stimulated 
wholesale  leasing  and  drilling  in  all  directions  in  Marion  county,  with 
the  result  that  a  small,  but  rich,  isolated,  field  of  about  three-fourths 
of  a  square  mile  was  denned.  This  field  is  still  credited  with  a  good 
production. 

A  new  gas  area  was  opened  in  1909  near  Carlinville.  Macoupin  county, 
by  the  Impromptu  Exploration  Company.  Several  wells  have  been 
drilled  south  of  the  town.  The  gas  comes  from  a  sandstone,  probably 
the  Pottsville,  immediately  above  the  Mississippian  limestones.  So  far, 
two  wells  have  produced  about  six  barrels  of  oil  per  day.  The  pressures 
of  gas  are  not  large  enough  to  warrant  an  extended  development  for 
commercial  purposes. 

A  small  gas  area,  similar  to  that  of  Carlinville,  was  also  opened  in 
the  spring  of  1910  several  miles  east  of  Jacksonville,  111.  The  wells 
were  small  in  quantity.  Late  in  1911  two  other  small  oil  wells  were 
added  to  the  field. 


16  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

In  April  of  1911  wild-catting  developed  an  oil  field  about  three  miles 
northwest  of  Carlyle,  111.,  which  has  since  been  defined  within  an 
area  of  about  iy2  square  miles.  The  governing  structure  of  the  field 
seems  to  be  an  elongated  dome  interrupting  the  gentle  trend  of  the 
broad  western  flank  of  the  Illinois  basin.  The  initial  production  of  the 
first  wells  was  excellent  and  caused  a  rush  to  the  territory.  High 
bonuses  were  paid  for  leases  many  miles  from  proven  territory  which 
later  proved  barren.  The  area  was  suggested  as  promising  by  the  State 
Geological  Survey  previous  to  exploitation.1 

Various  other  attempts  have  been  made  to  find  oil  at  widely  separated 
points.  Small  amounts  of  oil  or  gas  have  been  observed  in  such  lo- 
calities as  Mascoutah,  Marissa,  Waverly,  Greenville,  Decatur,  Iola,  Eldo- 
rado, Old  Eipley,  Patton,  Bartelso,  Bidgeway,  Campbell's  Hill,  and 
Denny.  Barren  wells  have  been  put  down  at  Herrick,  Cobden,  the 
American  bottoms  ea,st  of  St.  Louis,  Trenton,  Aviston,  Iuka,  Olney, 
Sumner,  Albion,  Carmi,  Duquoin,  Pinckneyville,  Coulterville,  Vandalia, 
Marshall,  Thomasboro,  Grafton,  Jerseyville,  Kane,  Bichview,  Nashville, 
Omaha,  Waterloo,  Hansen,  Pocahontas,  and  at  a  number  of  other  places. 

OBIGIN  AND  ACCUMULATION  OF  OIL. 
Origin  of  Oil. 

The  origin  of  oil  and  gas  has  been  a  puzzling  problem  for  many  years, 
especially  since  petroleum  has  come  into  world-wide  use.  Chemists  and 
geologists  have  attacked  the  problem  from  their  respective  points  of  view 
and  have  presented  plausible  theories,  none  of  which,  however,  have 
explained  satisfactorily  the  broad  distribution  of  petroleum  in  all  kinds 
of  sedimentary  rocks  of  various  ages. 

The  chemist  has  produced  many  of  the  component  parts  of  petroleum 
in  the  laboratory;  he  has  broken  down  certain  substances  into  constitu- 
ents, some  of  which  have  properties  resembling  those  of  crude  petroleum ; 
and  he  even  reproduced  certain  isometric  forms  of  hydrocarbons  peculiar 
to  petroleum — yet  the  theories  arising  from  these  results  fail  to  meet 
certain  geological  conditions  that  prohibit  their  acceptance. 

Geologists  have  met  the  problem  from  a  different  point  of  view.  Some, 
on  the  one  hand,  have  considered  the  conditions  of  deposition  of  sedi- 
mentary rocks  and  have  concluded  that  oil  and  gas  originate  from  animal 
and  plant  life  buried  in  the  sediments.  Others  have  conjectured  on  the 
internal  conditions  of  the  earth  during  its  stages  of  cooling  and  settling 
and  have  concluded  that  oil  originated  from  mineral  substances.  This 
attitude  is  closely  allied  to  the  chemist's  point  of  view.  The  geologist's 
views  are  not  wholly  acceptable  and  hence  the  origin  of  petroleum  re- 
mains uncertain.  The  whole  problem  has  resolved  itself  into  two  general 
theories  styled  the  inorganic  and  the  organic. 

THE  INORGANIC  THEORY. 

The  inorganic  theory  was  promoted  by  the  discovery  that  the  carbides 
of  certain  metals  may  be  broken  up  into  hydrocarbons  by  the  action  of 
water  and  that  alkaline  metals  produce  hydrocarbons  if  brought  into  con- 

i  Blatchley,  R.  S.,  111.  State  Geol.  Survey,  Bull.  No.  16,  pp.  87  and  167. 


blatchleyJ  ORIGIN"   AND   ACCUMULATION   OF   OIL.  17 

tact  with  water  saturated  with  carbon  dioxide  gas.  It  was  claimed  that 
volcanoes,  geysers,  and  hot  springs  indicate  heat  within  the  interior  of 
the  earth  sufficient  to  have  formed  carbides ;  and  that  these  were  broken 
up  by  percolating  waters  into  migrating  gases.  The  presence  of  hydro- 
carbons in  volcanic  gases  may  thus  be  explained.  Such  migrating  gases 
on  passing  from  hot  formations  to  higher,  cooler,  strata  would  naturally 
be  condensed  into  petroleum. 

It  is  claimed  that  granitic  rocks  are  full  of  joint  planes  and  other 
minute  cracks,  and  thus  it  is  impossible  for  the  gas  and  oil  to  remain  in 
them  because  of  the  ease  with  which  they  travel  and  diffuse.  When  the 
shales  are  reached  the  oil  "simplifies"  itself  or,  in  other  terms,  it  leaves 
more  or  less  of  its  more  viscuous  constituents  behind.  It  is  claimed  that 
the  oil  of  various  American  fields,  with  exception  of  those  like  the  Cali- 
fornia and  Texas  fields,  has  migrated  from  a  distance  to  the  localities  in 
which  they  now  are  found.  The  fact  that  all  oil  fields  are  confined  to 
sedimentary  strata  and  that  below  the  oil-bearing  horizons  there  fre- 
quently are  unproductive  strata  of  the  same  nature  makes  it  difficult  to 
understand  how  the  inorganic  theory  can  apply  to  our  larger  fields.  It 
is  difficult  to  understand  how  the  oil  of  such  fields  as  those  of  Pennsyl- 
vania and  Illinois  can  have  migrated  long  distances  and  not  left  traces 
of  travel  in  the  intervening  rocks.  It  is  apparent  that  the  inorganic 
theory  of  the  origin  of  oil  and  gas  is  open  to  many  criticisms.  The 
theories  derived  from  chemical  reactions  are  ingenious,  and,  no  doubt, 
may  explain  the  origin  of  some  petroleum;  they  do  not,  however  apply 
to  the  conditions  of  our  many  oil  fields  as  readily  as  the  organic 
theories. 

THE   ORGANIC   THEORY. 

The  organic  theory  advocates  that  oil  and  gas  originate  from  the 
decomposition  of  vegetable  or  animal  matter,  which  may  have  occurred 
in  the  bed  which  now  yields  oil  or  gas,  or  in  adjoining  beds  from  which 
they  have  migrated. 

Chemists  have  shown  that  when  the  body  of  an  animal  or  a  plant  is 
distilled  in  a  closed  retort  or  is  allowed  to  undergo  decay  in  the  absence 
of  air,  certain  gaseous  or  liquid  products  are  obtained,  which  resemble 
petroleum  and  natural  gas.  Much  the  same  results  are  obtained  by  bac- 
teriological putrefaction  of  organic  matter,  without  aid  of  heat.  Natural 
decomposition  of  animal  and  vegetable  matter  in  the  sedimentary  rocks 
through  the  periods  of  geologic  time  is  thought  to  explain  the  origin  of 
petroleum. 

Shale  is  held  to  be  the  source  of  petroleum  by  some  supporters  of  the 
organic  theory.  All  shale  beds  are  of  sedimentary  origin  and  are  com- 
posed of  fine  particles  of  clay.  The  clay  is  inorganic  and  was  deposited 
in  water  with  plants  and  marine  animal  life.  This  decomposition  was 
varied  by  the  deposition  of  sand,  and  limey  material.  The  completed 
stratified  rocks  comprise  a  succession  of  sandstone  and  limestone,  inter- 
lain  with  shale  beds.  In  some  fields,  as  California,  diatoms  embedded  in 
shale  are  regarded  as  the  source  of  the  oil.  Elsewhere  vegetable  remains, 
even  of  delicate  type,  like  algae,'  render  the  enclosing  shale  highly  bitu- 
minous and  oily.     It  is  thought  that  all  stratified  beds  contained  water 

—2  G 


18  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

in  some  degree  and  that  the  shales,  because  of  their  compactness,  had 
less  water  than  the  sands.  The  presence  of  water  in  the  formations 
may  have  aided  in  the  later  migration  of  the  oil  from  the  shales  to  the 
sands,  by  providing  a  ready  medium  through  which  the  oil  could  rise 
under  the  influence  of  gravity  to  the  highest  possible  position  in  the  sand 
strata.  The  shale  and  sand  oils  are  usually  classified  as  "sweet"  oils  in 
contradistinction  to  the  natural  petroleums  of  the  limestone  beds. 

The  limestone  theory  of  the  origin  of  oil  differs  from  the  last  by  sup- 
posing that  marine  animal  life,  peculiar  to  limestone  formations  was  the 
source  of  oil  in  the  sedimentary  rocks.  The  limestone  oils  of  Ohio, 
Indiana,  and  parts  of  Illinois  are  often  known  as  "sour"  oils,  because 
their  sulphur  and  nitrogen  content  is  greater  than  that  of  oils  found  in 
sand  formations.  They  have  a  ranker  odor  than  other  oils  and  are  often 
much  lighter  in  color;  in  fact,  they  are  sometimes  designated  as  "green" 
oils. 

The  oil  of  the  Mississippian  formations  or  the  Tracey  and  McClosky 
sands  have  undoubtedly  originated  from  marine  animals,  because  the 
producing  zones  are  highly  calcareous  sands  or  oolitic  limestones  and  the 
oil  contains  much  sulphur.  Some  of  the  oil  from  the  upper  Pennsyl- 
vanian  beds  in  Clark  county  is  sour  and  comes  from  calcareous  sand- 
stones. 

Of  the  two  organic  theories  of  the  origin  of  oil,  the  shale  theory  is 
the  more  applicable  to  the  pools  in  the  Pennsylvanian  or  "Coal  Measures" 
sands  of  the  Illinois  fields,  since  the  sands  seem  to  bear  few  or  no  fossils 
and  are  consequently  barren  in  animal  organic  remains.  There  was, 
however,  undoubtedly  a  great  abundance  of  plant  life  in  the  waters  of 
the  basin  of  southern  and  central  Illinois.  The  aquatic  plants  were 
algae  and  various  types  of  sea  weeds.  In  addition  to  these,  land  plants 
were  washed  down  by  streams  and  also  marsh  plants,  such  as  ferns, 
ground-pine,  etc.  Plants  from  both  sources  were  deposited  in  the  muds 
and  silts  of  the  accumulating  deposits  of  centuries.  These,  with  possibly 
some  marine  life,  were  shut  off  from  the  oxygen  of  the  air  and  other 
destructive  agents  and  were  trapped  within  the  shale  deposits,  where 
eventually,  through  the  lapse  of  geologic  time  a  peculiar,  slow,  distil- 
lation took  place,  wherein  the  protoplasm,  cellulose,  and  other  constitu- 
ents of  the  once  living  matter,  were  converted  into  oils  and  gases.  The 
distillation  and  migration  were  probably  a  matter  of  ages.  Natural  gas 
is  the  volatilized,  lighter  portion  of  the  oil  which  originated  according 
to  the  process  mentioned.  The  difference  of  gravity  between  gas,  oil, 
and  water  caused  the  two  former  substances  to  seek  the  highest  places 
in  the  rock  strata.  The  presence  of  natural  gas  in  any  area  is  generally 
accompanied  by  oil  at  some  point  along  the  structure  in  which  accumu- 
lation has  taken  place. 

Circulation  and  Accumulation  of  Oil. 

general  consideration. 

A  problem  of  special  importance  is '  the  circulation  of  oil  from  its 
source  and  its  mode  of  accumulation  in  porous  rocks.  The  matter  is 
being  investigated  by  laboratory  methods  by  various  scientists.     The  cir- 


blatchley]  ORIGIN    AXD    ACCUMULATION    OF    OIL.  19 

culation  is  accomplished  by  capillarity,  gravity,  and  gas  or  rock  pressure. 
The  accumulation  of  oil  requires  a  porous  reservoir  with  an  impervious 
cover  or  roof.  Certain  features,  of  geologic  structure  and  conditions  of 
water  saturation  are  important  factors  in  determining  the  localities  at 
which  the  accumulation  takes  place.  The  circulation  must  also  be 
affected  by  the  physical  properties  and  relations  of  the  oil  and  salt  water, 
and  the  rocks  in  which  they  occur.  One  of  the  potent  forces  in  directing 
the  circulation  is  doubtless  capillarity,  since  both  the  shales  and  the 
sands  are  porous  formations. 

Capillary  action  is  the  physical  phenomenon  consequent  upon  the 
attraction  or  repulsion  of  liquids  along  the  sides  of  very  fine  passages. 

If  a  liquid  of  low  specific  gravity  is  brought  into  contact  with  a  very 
fine  hair-like  tube  it  will  seemingly  pull  itself  along  the  passages;  while 
a  liquid  of  high  specific  gravity,  such  as  mercury,  will  exhibit  the  reverse 
tendency.  Capillary  attraction  is  accompanied  by  concave  liquid  sur- 
faces and  capillary  repulsion  by  convex  liquid  surfaces.  Prof.  A.  W. 
Duff,  of  the  AYorcester  Polytechnic  Institute  of  Massachusetts,  discusses 
the  effect  of  capillar}-  repulsion  and  attraction  as  follows:  "When  the 
effect  (of  capillary  action)  is  a  depression  (mercury),  the  depressed  sur- 
face is  curved  downward  and  the  tension  in  the  surface  provides  a  pres- 
sure. When  the  effect  is  an  elevation,  the  stretch  on  the  upward  curved 
surface  tends  to  draw  the  liquid  in  the  surface  layer  away  from  the 
liquid  below  and  so  produces  a  state  of  tension  or  diminution  of  pres- 
sure below  the  surface."  If  a  difference  of  capillarity  exists  between 
water  and  oil  in  small  tubes,  the  different  elevations  to  which  they  are 
raised  will  be  dependent  upon  the  differences  in  their  surface  tensions 
and  specific  gravities,  and  the  size  of  the  tubes. 

Shales  and  sandstones  are  porous  formations  containing  infinite  num- 
bers of  minute  spaces  capable  of  holding  liquid.  The  spaces  or  pores 
may  be  likened  to  capillary  tubes  and  may  be  assumed  under  proper 
conditions  to  promote  capillary  action.  William  Forstner1  has  the  fol- 
lowing to  say  of  the  classification  of  sand  interstices:  "The  interstices 
can  be  divided  into  three  classes :  openings  larger  than  those  of  capillary 
size,  capillary  openings,  and  openings  smaller  than  those  of  capillary 
size,  sub-capillary  openings.  Supercapillarity  openings  are  found  in  bed- 
ding and  joint  planes,  in  coarse  sandstones,  and  in  conglomerates.  In 
these  openings  the  flow  of  liquids  is  controlled  by  the  ordinary  laws  of 
hydrokinetics,  modified  by  the  viscosity  of  the  fluid,  and  the  regularity, 
size,  and  length  of  the  openings.  Capillary  openings  include  the  great 
majority  of  the  interstices  between  the  grains  of  sands  and  sandstones, 
many  of  those  in  conglomerates,  and  many  of  the  openings  caused  by 
fracture.  In  these  openings  the  velocity  of  flow  depends  upon  the  area 
and  cross-section  of  the  opening,  its  length,  and  the  viscosity  of  the  fluid. 
The  movement  is  so  slow  that  the  friction  of  the  moving  fluid  over  the 
sedimentary  film  is  very  small,  especially  in  long  openings.  Sub-capil- 
lary openings  include  part  of  the  interstices  in  coarser  sediments  having 
capillary  openings  and  nearly  all  the  interstices  between  the  grains  of 
clays,  shales,  and  slates.  The  movement  of  the  fluid  in  these  openings 
is  excessively  slow,  under  the  hydrostatic  pressures  generally  occurring 

i  Forstner,  William,  The  Occurence.of  Oil  and  Gas  in  the  South  Midway  Field,  Kern  County,  Cal- 
ifornia.   Economic  Geol.,  Vol.  VI,  1911,  p.  140. 


20  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

in  these  strata  the  movement  will  be  reduced  to  such  an  extent,  that  the 
fluid  may  be  considered  as  [existing  in]  fixed  films  held  by  molecular 
attraction." 

Capillarity  was  perhaps  effective  upon  the  included  water  of  shales 
long  before  the  distillation  of  oil  began  in  them,  and  may  have  caused 
the  expulsion  of  water  into  the  sands.  The  action  extended  to  the  oil 
which  began  to  originate  and  find  its  way  into  the  pores  of  the  shale. 
Its  production  was  exceedingly  minute,  yet  it  was  acted  upon  by  capil- 
larity, and  caused  to  ascend  toward  the  sand.  The  relation  of  specific 
gravity  of  oil  and  water  caused  the  oil  to  rise  to  the  top  of  the  water  in 
the  sandstones.  It  is  assumed  that  this  action  continued  as  long  as  dis- 
tillation took  place,  until  eventually  the  oil  had  left  the  shales  to  a  large 
degree  and  had  accumulated  in  the  sandstones.  The  action  may  have 
been  further  aided  by  various  compressions  of  the  formations  and  other 
unknown  physical  phenomena  until  the  shales  had  given  up  most  of  their 
oil  to  adjoining  porous  sandstones. 

It  is  probable  that  the  gaseous  hydrocarbons  and  petroleums  of  various 
specific  gravities  were  not  separated  until  the  more  porous  beds  were 
reached.  Under  the  stress  of  earth  movements  and  different  degrees  of 
heat  and  pressure,  changes  in  the  composition  of  the  petroleums  must 
have  occurred.  Again  the  oil  may  have  been  affected  chemically  by 
water  in  the  sandstones  and  altered  from  its  original  condition. 

It  is  apparent  that  the  distribution  of  petroleum  is  greatly  influenced 
by  the  presence  of  water  and  it  is  a  fact  that  there  is  abundant  water 
in  the  Illinois  oil  sands.  Oil  is  lighter  than  water.  If  both  are  present 
the  oil  rests  upon  the  surface  of  the  water  and  is  to  that  extent  con- 
trolled by  the  latter.  If  oil  and  water  are  not  associated,  the  petroleum 
moves  downward  along  bedding  planes  and  through  coarse,  porous  strata 
under  force  of  gravity.  In  such  a  case  it  may  occur  in  pores  at  the 
bottom  of  a  syncline. 

A  third  theoretical  agent  of  the  circulation  of  oil  from  its  source  of 
distillation  to  its  present  position  is  perhaps  that  of  gas  pressure  or 
"rock  pressure."  This  pressure  is  always  noticeable  when  a  new  oil  or 
gas  area  is  opened  up.  The  oil  generally  rises  far  up  into  the  casing 
of  the  new  well  and  often  above  its  mouth.  If  gas  is  present  and  the 
casing  is  closed  so  that  the  product  cannot  escape  into  the  air,  a  pressure 
is  developed  inside  the  pipe.  The  gas  may  accumulate  instantly  and 
thus  indicate  a  very  porous  reservoir  beneath,  or  it  may  take  consider- 
able time  to  gather  and  thus  show  a  less  porous  one.  The  two  conditions 
have  often  occurred  in  the  same  locality  and  yet  the  same  pressures  were 
eventually  secured.  It  is  thought  that  gas  pressure  may  help  to  pro- 
mote movement  of  oil  through  the  containing  rocks. 

New  lines  of  investigation  have  been  carried  on  recently  by  Dr.  D.  T. 
Day,  J.  Elliot  Gilpin,  and  Oscar  E.  Bramsky  of  the  United  States 
Geological  Survey  in  an  effort  to  find  the  cause  of  the  differences  be- 
tween such  oils  as  those  of  Pennsylvania  and  Illinois  and  those  of  Ohio 
and  Indiana,  or  rather  the  Trenton  limestone  oils.1  The  question  reverts 
to  the  cause  of  the  difference  between  "sweet"  and  "sour"  oils,  assuming 
that  all  petroleum,  no  matter  what  its  source  is,  is  a  definite  substance ; 

1  Gilpin,  J.  Elliott,  and  Bramsky,  Oscar  E.,  The  Diffusion  of  Crude  Petroleum  through  Fuller's  Earth, 
Bull.  U.  S.  Geo  1.  Survey  No.  475,  1911. 


blatchley]  ORIGIN"   AND   ACCUMULATION   OF   OIL.  21 

the  product  of  one  field  differing  from  another  only  in  the  proportion  of 
its  series  and  members  of  hydrocarbons.  The  Pennsylvanian  and  Illi- 
nois "sweet"  oils  are  found  to  contain  a  larger  proportion  of  paraffin 
hydrocarbons  and  less  benzine,  unsaturated  hydrocarbons,  sulphur  and 
nitrogen  than  the  Ohio  and  some  California  oils.  It  is  concluded  that 
the  first  mentioned  oils  were  migratory,  because  the  sands  in  which 
they  are  found  bear  little  evidence  of  containing  a  source  for  the 
petroleum,  while  the  oils  of  Ohio  and  perhaps  the  McClosky  oil  of  the 
Illinois  fields  are  thought  to  have  originated  in  the  limestone  beds  in 
which  they  are  found.  If  such  is  the  case  and  petroleum  is  everywhere 
the  same  substance  except  for  the  lack  of  certain  hydrocarbons,  the 
difference  in  the  two  grades  of  oil  must  be  the  result  of  migration 
through  filtrating  materials,  or,  in  other  words,  of  a  "selective  activity" 
of  shale  or  clay.  It  may  be  true  that  some  of  the  Pennsylvania  and 
Illinois  oils  now  reposing  in  sands  were  originally  of  animal  origin  and 
they  have  lost  some  of  their  original  ingredients  by  migration.  These 
conclusions  led  to  experiments  upon  the  diffusion  of  petroleum  through 
Fuller's  earth,  which  is  a  good  type  of  shale  for  purposes  of  investiga- 
tion. It  was  found  by  Day  that  oil  such  as  the  Illinois  oil  could  be 
produced  by  this  method  from  crude  Trenton  limestone  oil.  Glass  tubes 
packed  with  dry  Fuller's  earth  were  placed  in  vessels  containing  crude 
Illinois  oil.  The  oil,  in  the  course  of  some  time,  began  to  move  up- 
ward in  the  tubes  by  force  of  capillarity.  Examination  of  the  tubes  at 
the  conclusion  of  the  migration  showed  that  light  oils  were  found  at 
the  top,  and  low  grade,  heavy  oils,  sulphur,  and  other  heavy  constituents 
at  the  bottom  of  the  tube.  Continued  nitrations  of  the  oil  removed  the 
sulphur  compounds  entirely. 

It  was  concluded  from  these  experiments,  "that  the  Illinois  oil  at 
some  time  in  its  history  diffused  through  porous  media,  which  exercised 
a  selective  action  upon  it,  removing  a  large  part  of  the  unsaturated  and 
sulphur  compounds  and  probably  the  benzine  and  nitrogen  compounds." 


THE  POROUS  STRATUM. 

Petroleum  was  valueless  as  a  commercial  product  when  it  was  origi- 
nally formed,  because  its  diffusion  was  so  complete  that  a  bore  into  the 
containing  rock  could  scarcely  have  obtained  a  showing  of  oil.  Its  ac- 
cumulation in  pools  of  -commercial  value  first  demands  more  porous 
beds  than  the  shales  in  which  it  is  supposed  to  have  originated.  The 
strata  of  sand  interlain  with  the  shales  are  suitable  reservoirs  because 
in  most  cases  they  are  much  more  porous  than  the  compact  shales. 
Exceptionally,  the  sands  themselves  contain  portions  which  are  extremely 
compact  and  impervious.  These  non-porous  areas  may  act  as  retaining 
covers  and  effect  the  concentration  of  underlying  oil  where  structure  is 
favorable.  They  may  be  extensive  enough  to  separate  adjoining  pools, 
or  they  may  be  small  enough  in  extent  to  cause  mere  local  "dry  spots" 
in  the  midst  of  very  productive  territory,  in  which  the  sands  are  other- 
wise highly  porous.  The  presence  of  small  streaks  of  shale  within  the 
sandstones  is  frequent  in  Illinois  formations.  Often  two  or  three  aver- 
aging 5  to  15  feet  in  thickness  may  occur  in  a  thickness  of  50  to  80 
feet  of  sancl.     The   driller  terms  these  "breaks."     The  sand   and  the 


'?•?  OIL  FIELDS  OF  CRAWFORD  AXD  LAWRENCE  COUNTIES.    [BUM*  NO.  22 

*T>reak"  merge  into  one  another  in  most  cases  and  oil  is  not  often  found 
where  sand  and  shale  are  thus  mixed. 

IMPERVIOUS   COYER. 

Aii  important  requirement  for  the  accumulation  of  oil  and  gas  is  an 

impervious  cover,  or  retaining  roof,  which  will  hold  the  oil  and  gas  cap- 
tive in  the  porous  stratum.  In  Illinois  there  is  almost  invariably  a 
cover  of  hard,  compact,  shale  over  the  oil  sands.  This  is  particularly 
true  of  the  sands  in  the  Pennsylvanian  formations.  The  producing  sands 
in  the  Mississippian  formations  are  overlain  in  some  instances  by  lime- 
stone. The  impervious  covers  have  doubtless  caused  the  retention  of 
the  oil  in  the  sands  during  the  periods  of  earth  movements  which  caused 
structural  folds  in  the  rock.  If  an  oil  pool  did  not  have  an  impervious 
cover  between  it  and  the  surface,  the  lighter  portions  of  the  oil  would 
long-since  have  volatilized  and  passed  off  as  natural  gas,  while  only 
the  heavy  oil  or  asphalt-like  residue  would  remain.  Where  a  thin  cover 
lies  over  a  productive  oil  sand  some  of  the  lighter  portions  of  the 
petroleum  have  escaped  and  heavy,  lubricating  oil  is  generally  found. 
This  is  of  low  gravity  and  consequently  of  low  grade,  and  generally 
serves  as  fuel  oil.  The  abundance  of  shales  within  the  "Coal  Measures" 
and  the  upper  Mississippian  rocks  of  Illinois  have  prevented  an  ex- 
tensive volatilization  and  consequently  the  oils  are  of  good  grade,  aver- 


GEOLOGICAL  STRUCTURES. 

Another  very  important  necessity  for  the  accumulation  of  oil  and  gas 
in  pools  is  the  presence  of  certain  types  of  structural  features  in  the 
rocks.  The  sedimentary  strata  were  deposited  under  water  horizontally, 
or  practically  so.  and  the  natural  distillation  of  oil  probably  took  place 
primarily  while  the  beds  were  in  that  position.  Subsequent  disturbances 
took  place  causing  the  strata  to  be  folded,  forming  as  it  were,  arches3  or 
domes,  in  some  places,  and  corresponding  troughs  or  basins  in  others. 
The  arches  are  known  as  anticlines  while  the  troughs  are  called  synclines. 
When  these  undulations  took  place,  the  water,  petroleum,  and  gas  within 
the  sand  formations  were  forced  to  move  and  distribute  themselves 
according  to  the  laws  of  gravitation  and  hence  according  to  their  specific 
gravities.  The  water  was  the  heaviest  of  the  three  fluids,  and,  therefore, 
sought  the  synclines  as  far  as  possible,  depending,  of  course,  upon  the 
porosity  of  the  sands.  Its  tendency  was  to  displace  the  oil  and  gas, 
forcing  the  oil  to  float  on  the  water  and  the  gas  to  rise  still  higher.  The 
oil  was  enabled  to  rise  as  far  as  the  water  extended  up  the  slopes  of  the 
syncline,  while  the  gas  was  able  to  free  itself  from  the  fluids  and  rise 
to  the  highest  place  in  the  porous  bed,-  usually  the  crests  of  the  anti- 
clines. 

The  earth  disturbances  effecting  the  changes  in  the  positions  of  the 
strata  may  be  responsible  also  for  minor  irregularities  which  occur  on 
the  anticlines  and  synclines  themselves.  The  surface  of  an  oil  sand  on 
the  anticline  may  be  pitted  or  undulating.  This  condition  may  affect  an 
extensive  area  or  only  a  few  acres  of  ground.  The  general  accumulation 
of  oil  and  gas  is  governed  by  the  anticline  proper,  covering  many  miles, 
and  the  segregation  of  pools  may  possibly  be  caused  by  smaller  folds  on 


blatchley]  ORIGIN   AND    ACCUMULATION    OF    OIL.  23 

the  large  one.  Coupled  with  this  intricate  system  of  synclines  and 
arches  on  the  parent  fold,  there  is  variation  in  the  porosity  of  the  sands ; 
the  two  conditions  greatly  affect  the  distribution  of  oil  and  gas.  It  is 
readily  recognized  that  either  factor  may,  locall}-,  explain  the  presence 
of  dry  holes  within  productive  territory.  Some  question  has  arisen  as 
to  whether  these  minor  arches  are  true  anticlinals  of  deformational 
character  or  whether  they  represent  merely  original  thickening  and 
thinning  of  particular  beds  or,  again,  whether  they  result  from  unequal 
settling  during  the  consolidation  of  the  sediments.  Locally,  any  or  all 
of  these  factors  may  account  for  the  conditions. 

Another  important  type  of  geologic  structure  in  which  an  accumula- 
tion often  occurs,  is  the  "terrace"  or  flattened  area  upon  the  flanks  of 
a  syncline  or  anticline.  The  terrace,  strictly  speaking,  is  an  interrup- 
tion in  the  uniform  dip  of  the  sides  of  a  basin,  where  the  rocks  are 
approximately  horizontal.  Such  terraces  are  to  be  found  upon  the  sides 
of  the  great  structural  basin  in  southern  and  central  Illinois.  A  segre- 
gation of  oil  takes  place  upon  a  favorable  terrace  much  in  the  same 
manner  as  in  the  anticlines  and  the  synclines.  The  water  of  the  basin 
enables  the  oil  to  rise  to  the  terrace,  where  it  may  be  trapped  by  friction. 
But  the  oil,  originally  in  the  sloping  sand  above  the  terrace,  may  migrate 
farther  up  the  general  incline  so  as  to  float  on  the  water  surface.  The 
gas  follows  its  usual  course  in  freeing  itself  from  the  oil  and  accumu- 
lates in  the  terrace  head  or  continues  up  the  general  dip  to  the  adjacent 
anticline  or  to  some  impervious  barrier. 

Frederick  G.  Clapp  has  classified  oil  pools  according  to  their  geo- 
logical structure,  because  all  known  fields  have  shown  their  accumula- 
tions to  be  due  primarily  to  definite  structures.  His  classification  is  as 
follows  •} 

1.  When  anticlinal  and  synclinal  structure  exists. 

Strong  anticlines  standing  alone. 

Well  defined  alternating  anticlines  and  synclines. 

Monoclines  with  change  in  rate  of  dip. 

Structural  terraces. 

Broad  geanticlinal  folds. 

2.  Quaquaversal  structures. 

Anticlinal-bulge  type. 
Saline  dome  type. 
Volcanic  neck  type. 

3.  Along  sealed  faults. 

4.  Oil  and  gas  sealed  in  by  asphaltic  deposits. 

5.  Contact  of  sedimentary  and  crystalline  rocks. 

6.  In  joint  cracks  of  sedimentary  rocks. 

7.  In  crystalline  rocks. 

Investigations  of  the  main  fields  in  Lawrence  county,  Illinois,  reveals 
an  additional  member  to  Clapp's  arrangement.  This  is  a  double  plung- 
ing anticline  or  a  combination  of  a  strong  anticline  standing  alone  and 
a  dome  or  quaquaversal  structure.  This  may  fall  under  Class  I  or  it 
may  necessitate  subdivision  of  Class  2  as  follows: 

2.     Quaquaversal  structures. 

(a)  Anticlinal-bulge  type. 

(b)  Saline  dome  type. 

(c)  Double-plunging  anticline  type. 

(d)  Volcanic  neck  type. 

i  Clapp,  Frederick  G.,  The  Occurence  of  Oil  and  Gas  Deposits  Associated  with  Quaquaversal  Struc- 
ture.   Economic  Geology,  Vol.  VII,  No.  4, 1911,  p.  364-381. 


24  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 

WATER  SATURATION. 

One  of  the  most  important  factors,  if  not  the  greatest,  in  the  concen- 
tration of  oil  in  raised  structures,  is  the  presence  or  absence  of  water  in 
the  oil-bearing  stratum.  Mr.  W.  T.  Griswold  offers  some  very  interesting 
observations  upon  this  subject  with  reference  to  the  Appalachian  region.1 
The  theories  are  more  or  less  applicable  to  the  Illinois  rocks,  inasmuch 
as  they  are  of  similar  age  and  character.    His  conclusions  are  as  follows : 

"In  dry  rocks  the  principal  points  of  accumulation  of  oil  will  be 
at  or  near  the  bottom  of  the  syncline  or  at  the  lowest  point  of  the  porous 
medium,  or  at  any  point  where  the  slope  of  the  rock  is  not  sufficient  to 
overcome  the  friction,  such  as  structural  terraces  or  benches.  In  porous 
rocks,  completely  saturated,  the  accumulation  of  both  oil  and  gas  will 
be  in  the  anticlines  or  along  level  portions  of  the  structure.  Where  the 
area  of  porous  rocks  is  limited,  the  accumulation  will  occur  at  the 
highest  point  of  the  porous  stratum;  and  where  areas  of  impervious 
rocks  exist  in  a  generally  porous  stratum  the  accumulation  will  take 
place  below  such  impervious  stop,  which  is  really  the  top  limit  of  the 
porous  rock.  In  porous  rocks  that  are  only  partly  filled  with  water  the 
oil  accumulates  at  the  upper  limit  of  the  saturated  area.  This  limit  of 
saturation  traces  a  level  line  around  the  sides  of  each  structural  basin, 
but  the  height  of  this  line  may  vary  greatly  in  adjacent  basins  and  in 
different  sands  of  the  same  basin. 

"Partial  saturation  is  the  condition  most  generally  found,  in  which 
case  accumulations  of  oil  may  occur  anywhere  with  reference  to  the  geo- 
logic structure.  It  is  most  likely,  however,  to  occur  upon  terraces  or 
levels,  as  these  places  are  favorable  to  accumulation  in  both  dry  and  sat- 
urated rocks. 

"Under  all  conditions  the  most  probable  locations  for  the  accumula- 
tion of  gas  are  on  the  crests  of  anticlines.  Small  folds  along  the  side 
of  a  syncline  may  hold  a  supply  of  gas,  or  the  rocks  may  be  so  dense  that 
gas  mav  not  travel  to  the  anticline,  but  will  remain  in  volume  close  to 
the  oil." 

The  above  observations  were  found  applicable  in  the  Illinois  oil  fields, 
as  described  under  the  relations  of  structure. to  salt  water,  oil  and  gas. 
The  Illinois  wild-cat  areas  have  not  offered  sufficient  data  as  to  water 
saturation  to  warrant  conclusions  with  reference  to  it.  It  is  hoped  that 
in  the  future  the  operators  in  Illinois  will  note  with  as  much  exactness 
as  possible  the  wet  condition  of  the  sands  they  encounter.  It  will  then 
be  possible  for  the  geologist  or  engineer  to  offer  better  suggestions  as  to 
the  probable  conditions  in  prospective  oil  areas. 

GENERAL  GEOLOGY  OF  ILLINOIS  RELATING  TO  OIL  AND 

.     *  GAS. 

Introduction. 

In  order  that  the  reader  may  have  a  general  view  of  the  oil  and  gas 
conditions  of  the  State,  a  brief  elementary  review  of  its  geology  is  pre- 
sented. 


i  Griswold,  W.  T.  and  Munn,  M.  J.,  Geology  of  Oil  and  Gas  Fields  in  Steuben ville,  Burgettstown 
and  Claysville  Quadrangles,  Ohio,  West  Virginia  and  Pennsylvania.  Bull.  U.  S.  Geol.  Survey  No.  318, 
1907,  p.  15. 


blatchley]  GEOLOGY    OF    ILLINOIS.  25 

Those  who  have  observed  the  ledges  exposed  at  quarries  or  in  the 
banks  of  streams  appreciate  that  the  rocks  occur  in  rather  definite  layers 
of  varying  thickness.  Well  drillers,  especially,  realize  that  sandstone, 
shale,  limestone  and  combinations  of  these  rocks  underlie  the  State  as 
alternating  strata  of  considerable  regularity.  The  study  of  these  rela- 
tions constitutes  stratigraphic  geology  or  stratigraphy. 

A  rock  stratum  may  underlie  a  large  or  a  small  area.  Thus,  a  coal 
bed  or  an  oil  sandstone,  or  "sand,"  may  be  present  in  one  locality  but 
absent  in  the  adjoining  region.  The  a/real  extent  of  oil  sands  therefore 
is  a  matter  of  importance  to  operators. 

The  rock  layers  exposed  to  view  appear  to  be  flat-lying  or  horizontal. 
Detailed  study  may  show  gentle  pitching  or  dipping  of  the  strata.  Thus, 
a  sandstone  may  lie  300  feet  below  sea  level  in  a  particular  area,  but 
dip  so  as  to  be  500  feet  below  sea  level  in  an  adjoining  county.  Excep- 
tionally, the  rocks  lie  in  gentle  folds.  The  attitude  or  "lie"  of  the  strata 
constitutes,  broadly,  their  "structure;"  and  the  determination  of  this  is 
of  utmost  importance  in  the  discovery  and  development  of  an  oil  field. 

The  geology  of  the  State  is  described  elsewhere1  in  a  more  detailed 
manner;  it  will  be  sufficient  in  this  report  to  discuss  its  significant  fea- 
tures, briefly,  under  the  headings  just  mentioned. 


Stratigraphy. 

The  accompanying  sections  indicating  the  order  and  character  of 
the  strata  were  first  published  by  Bain2  in  1907.  They  are  modified  by 
the  writer  to  agree  with  later  data  and  conclusions. 

Overlying  the  consolidated  rocks  of  the  State  except  in  the  extreme 
southern  and  the  northwestern  counties,  there  is  a  varying  thickness  of 
glacial  deposits  or  "drift"  These  clays,  sands,  gravels,  etc.,  are  com- 
monly encountered  in  drilling  before  hard  rock  is  reached.  Locally,  they 
contain  gas  and  Bain  says: 

"Natural  gas  is  found  in  these  deposits  in  small  quantity  at  a  number 
of  points  throughout  the  State.  Such  wells  are,  or  have  been,  known 
near  Champaign,  Princeton,  Colchester,  Wapella,  Heyworth,  and  else- 
where. The  pressure  is  usually  slight  and  the  life  of  the  individual 
wells  is  usually  short.  While  it  is  not  possible  in  every  case  to  absolutely 
exclude  the  possibility  of  these  wells  representing  leakage  from  lower 
reservoirs,  a  sufficient  explanation  of  them  is  believed  to  be  found  in 
the  decay  of  woody  material  buried  in  the  drift  itself.  These  wells  are 
characteristically  difficult  to  maintain  owing  to  sand  clogging  the  pipes." 

The  section  for  southern  Illinois  is  most  important  in  the  present 
study.  The  formations  yielding  oil  and  gas  production  are  indicated 
by  italic  and  occur  chiefly  in  the  Carboniferous  system.  Possible  oil 
"sands"  are  suggested  also  in  the  Ordovician  and  Silurian  systems, 
especially  in  central  and  northern  Illinois. 

i  Weller,  Stuart,  The.  Geological  Map  of  Illinois:    Bull.  111.  State  Geol.  Survey  No.  6,  1907. 

2  Bain,  H.  Foster,  Petroleum  Fields  in  Illinois  in  1907:    Bull.  111.  State  Geol.  Survey  No.  8,  pp.  273-312. 


<?i; 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


Northern  Illinois  section. 

This  section  is  intended  to  be  representative  for  that  portion  of  the  State 
lying  north  of  Rock  Island,  LaSalle,  and  Kankakee. 


f  McLeansboro.    Limestones  and  nodular  calcareous  shales  in  upper  part  and  sand- 
I       stone  at  the  base.    Thickness  300  feet. 

Pennsylvanian.  \  Carbondale.    Coal,  shale,  sandstone  and  limestone.    Thickness  200  feet. 

|  Pottsville.    Shale.    Thickness  2  to  20  feet. 

{  TJnconforn  ity. 


Devonian 


Silurian. 


Ordovician. 


f  Limestone.    Thickness  125  feet. 
\  Unconformity. 

\  Niagara.    Dolomite.    Thickness  20  to  400  feet. 
i      in  the  vicinity  of  Chicago. 
I  Unconformity. 


Contains  frequent  seepages  of  bitumen 


Cincinnatian  (Maquoketa).    Shales  and  limestone. 
Thickness  50  to  225  feet. 
Unconformity. 

Galena-Trenton.    Mainly  dolomite;  a  little  limestone  and  shale  at  the  base.    Thick- 
ness 230  to  450  feet.    A  very  persistent  "oil  "rock  or  petroliferous  shale  in  the  lower 

portion. 
St.  Peter.    Sandstone,  friable.    Thickness  100  to  220  feet.    Heavily  water-bearing. 
Lower  Magnesian.  Dolomitic  limestone.  Penetrated  to  845  feet.  All  but  upper  part 

known  from  well  records;  rests  on  Potsdam  sandstone,  known  only  from  well  records. 


Central  Illinois  section. 

For  the  region  south  of  Rock  Island,  LaSalle,  and  Kankakee,  and  north  of 
the  Missouri  river  and  Marshall,  Clark  county. 


Pennsylvanian. 


Mississippian. . 


Devonian. 


McLeansboro.    Shales,  sandstones,  thin  limestones  and  coals.    Rocks  between  top 

of  Herrin  (No.  6)  coal  and  bed  rock.    Thickness  125  to  700  feet. 
Carbondale.      Coals,   shales  and  sandstones.      Rocks  between  the  base  of  the 

Murphysboro  (No.  2)  coal  and  the  top  of  the  Herrin  Coal.      Thickness  100  to 

300  feet. 
Pottsville.    Sandstones,  thin  shales  and  coals.    Thickness  150  to  200  feet.     Carlin- 

ville  oil-sand,  Macoupin  county;  small  amounts  of  oil  and  gas  reported  but  position 

not  certain. 
Unconformity. 

Birdsville  and  Tribune  (Chester).  Irregular  thickness  of  sandstone,  shale  and 
limestone,  recognized  in  a  few  borings;  generally  absent  in  this  territory .  Thick- 
ness 0  to  50  feet. 

Ste.  Genevieve,  St.  Louis,  and  Salem.  Limestone,  non-magnesian,  partly  cherty 
and  partly  oolitic.    Thickness  225  to  400  feet. 

Osage  (Burlington,  Keokuk  and  Warsaw).  Shales  and  limestone,  the  latter  often 
cherty.   Thickness  100  to  400  feet.    Crude  petroleum  in  geodes  near  top  of  the  Keokuk . 

Kinderhook.    Shales,  limestones,  and  sandstones.    Thickness  40  to  120  feet. 
I  Unconformity. 

f  Upper  Devonian.    Shale.    Thickness  0  to  130  feet. 
Hamilton.    Limestones.    Thickness  0  to  100  feet. 
I  Unconformitv. 


Gas  at  Pittsfield,  Pike  county  and 


„..     .  /  Niagara.    Dolomite.    Thickness  50  to  150  feet, 

biiunan ^      oil  seepage  in  Calhoun  county. 

f  Cincinnatian  (Maquoketa).    Shales.    Thickness  40  to  200  feet. 
[   Unconformity. 
Ordovician..*.  \  Galena-Trenton.   Dolomite.   Thickness  200  to  400  feet.   Oil  seepage  in  Calhoun  county. 
I   St.  Peter.    Sandstone.    Thickness  120  to  170  feet.    Lower  Magnesian.    Dolomitic 
I      limestone.    Penetrated  to  700  feet. 


Southern  Illinois  section. 

For  the  area  lying  south  of  a  line  drawn  eastward  from  the  mouth  of  the 
Missouri  river  to  Marshall,  Illinois,  and  the  State  line. 


Quaternary . 
Tertiary 


J  Glacial  till,  sand,  and  gravel;  loess  and  alluvium.    Present  as  surface  rocks  every- 

■  •  \  where  except  in  northwest  and  extreme  south.      Thickness,  30  to  225+  feet. 

J  Lafayette,  LaGrange  and  Porters  Creek.    Clays,  sands,  gravel,  and  ferruginous 

■  -  \      conglomerate.    Occurs  only  in  extreme  south.    Thickness  250  feet. 


Cretaceous <      feet 


Clay  and  sand.      Occurs  only  in  extreme  south.      Thickness  20  to  40 


BLATCHLEY] 


GEOLOGY    OF    ILLINOIS. 


27 


Pennsylvania!!. 


Mississippian 


Devonian . 


Silurian. 


Ordovician  .. 


Southern  Illinois  Section — Concluded. 

McLeansboro  formation.  Shales,  sandstones,  thin  limestones  and  coals.  Rocks 
between  top  of  Herrin  (No.  6)  coal,  and  bed  rock.  Thickness  500  to  1,000  feet. 
Contains  the  oil  and  gas  sands  of  £hc  Westfield,  Siggins  and  Casey  pools. 

Carbondale  formation.  Coals,  shales  and  sandstones.  Rocks  between  the  base 
of  Murphysboro  (No.  2)  coal  and  the  top  of  the  Herrin  coai.  Thickness  about  375 
feet.    Lower  "pay,"  Johnson  township  pool,  Clark  county. 

Pottsville  formation.      Sandstone,    some  thin  shales  and  coals.      Thickness  300 
to  700  feet.      Includes  the  Buchanan  sand  (base),  and  Bridgeport  sand  (top),  Law- 
rence county:  Robinson  sand  (top),    Crawford  county;  oil  sand  of  Litchfield,  Mont- 
gomery county:  probably  the  Princeton,  Ind.,  oil  sand. 
'[  Unconformity. 

Birdsville  and  Tribune  (Chester).    Sandstones,  shale,  and  limestones;  usually  six 

limestones  with  three  well  defined  beds  (non-cherty)  and  generally  with  red  shale 
at  the  base.  Thickness  770  feet.  "Gas"  and  Kirkwood  sands,  Lawrence  county; 
gas  sand,  Vincennes,  Ind.;  Sparta  sand,  Randolph  county;  Stein  and  Benoist  sands, 
Marion  county  (the  latter  is  the  equivalent  of  the  Kirkwood  sand);  Lindley  gas  sand, 
Bond  county:  Carlyle  sand,  Clinton  county  and  the  Oakland  City  sand,  Pike  county, 
Ind.  Tracey  sand,  Lawrence  county  and  probably  Denny  sand,  Perry  county  (show 
of  oil. 

Cypress.  Sandstone,  massive,  coarse-grained;  fairly  regular  in  a  thickness  of  80 
to  150  feet  in  southwestern  Illinois;  very  irregular  and  usually  thin  in  southeastern 
Illinois.    The  Cypress  sandstone  is  absent  in  the  oil  fields  of  Lawrence  county. 

Unconformity. 

Ste.  Genevieve.  Limestone,  mostly  oolitic  and  very  cross-bedded.  Thickness,  80 
to  100  feet.     Mc  Closky  sand,  Lawrence  county. 

St.  Louis  and  Salem  (Spergen).  Limestone,  dense  becoming  oolitic  in  lower  divi- 
sion. Thickness  320  feet.  Show  of  oil  reported  at  base  in  the  Lawrence  county  pool 
near  Bridgeport. 

Osage  (Burlington,  Keokuk  and  Warsaw).  Shale  above  and  coarse-grained  lime- 
stone with  chert  below.    Thickness  440  feet. 

Kinderhook.    Shale  and  shaly  limestone,  red.    Thickness  60  feet. 

f  Upper  Devonian  (Sweetland  Creek).    Shale.    Thickness  50  to  60  feet. 

|  Hamilton.    Limestone.    Thickness  about  100  feet. 

\  Onondaga  (Grand  Tower).    Limestone.    Thickness  155  feet. 

f  Oriskany  (Clear  Creek).    Chert  and  limestone.    Thickness  200  to  240  feet. 

{  Helderberg  (New  Scotland).    Limestone.    Thickness  165  feet. 


/  Alexandrian  (Sexton  Creek,  Edgewood  and  Girardeau) 
1      Thickness  116  feet. 


Limestone,  some  shale. 


Richmond  (Cincinnatian).    Orchard  Creek,  shale,    Thebes  sandstone,    Fernvale 

limestone .    Thickness  about  100  feet. 
Galena-Kimmswick.    Non-dolomitic  limestone.    Thickness  510  feet  recorded. 

St.  Peter.    Sandstone.    120  feet  recorded. 
Lower  Magnesian.    Mostly  dolomitic  limestone  with  occasional  thin  layers  of  sand 

and  shale.    545  feet  recorded. 


Areal  Extent  of  the  Formations  and  Oil  Sands. 


The  extent  of  the  main  geologic  systems  in  Illinois  is  suggested  by  the 
map  already  published.1  Of  particular  interest  here  is  the  extent  of  the 
formations  which  are,  or  may  be,  productive  of  oil  and  gas.  Passing 
from  the  youngest  to  the  oldest  or  lowest  rocks,  by  far  the  most  important 
are  the  Pennsylvanian  and  Mississippian  formations ;  although  the  Silur- 
ian and  Ordovician  rocks  deserve  brief  mention.  The  Carboniferous  in- 
clude the  Pennsylvanian  ("Coal  Measures")  series  and  the  underlying 
Mississippian. 

The  Pennsylvanian  rocks  occupy  42,000  square  miles  in  the  heart  of 
Illinois.  They  are  absent  from  that  part  of  the  State  lying  north  of  an 
irregular  line  drawn  eastward  from  Eock  Island.  The  boundary  swings 
southward  from  near  the  mouth  of  Kankakee  river  to  a  point  west  of 
Paxton,  thence  northeast  to  the  State  line  near  Watseka.  South  of  this 
line  the  Pennsylvanian  rocks  continue  from  Illinois  into  Indiana  and 
Kentucky.  The  southern  and  western  margins  of  the  area  follow  the 
trend  of  the  Ohio  and  the  Mississippi  at  a  distance  of  10  to  25  miles. 
The  Pennsylvanian  rocks  of  the  southern  area  are  thickest  and  most 

i  Loc.  cit. 


28  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 

complete.  They  are  thinner  in  the  central  section,  chiefly  because  of  the 
thinning  away  of  the  Pottsville  formations  with  their  included  oil  sands. 
North  and  northwest  of  Springfield  these  rocks  are  essentially  absent 
but  they  are  present  eastward  from  Decatur.  A  thin  layer  occurs  also  in 
the  vicinity  of  Rock  Island.  The  lowest  beds  of  the  Pennsylvanian  are 
lacking  along  the  western  boundary  of  the  State  from  Randolph  county 
northward  to  Rock  Island.  It  thus  appears  that  the  oil  sands  of  the 
Pottsville  are  most  promising  in  the  central  and  southeastern  parts  of 
the  State.  Even  there,  the  Pottsville  may  be  limited  to  areas  from  which 
the  upper  Chester  formations  have  been  eroded.  The  higher  sands  may 
be  found  present  practically  anywhere  except  at  the  thin  edge  of  the 
Pennsylvanian  area.  "The  horizontal  extent  of  the  various  sands  is  not 
known  accurately,  even  within  the  drilled  areas,  because  of  lack  of  good 
well  records  and  consequent  difficulty  of  identifying  the  sands. 

The  Pennsylvanian  rocks  above  the  Pottsville  are  subdivided  into 
upper  and  middle  parts,  the  Pottsville  constituting  the  basal  portion. 
The  upper  part  is  specifically  known  as  the  McLeansboro  and  the  middle 
part,  the  Carbondale. 

The  McLeansboro  formation  includes  all  the  rocks  between  the  top  of 
the  Herrin  or  No.  6  coal  and  the  top  of  the  Pennsylvanian  series.  A 
thin  layer  of  shale  usually  overlies  the  Herrin  coal  followed  by  a  very 
persistent  limestone.  The  limestone  contains  a  small  fossil  known  as 
the  Fusulina,  which  is  about  the  size  of  a  large  grain  of  wheat.  It 
tapers  at  both  ends  and  a  cross-section  has  the  appearance  of  concentric 
circles.  Dr.  Udden  has  been  able  to  distinguish  fragments  of  the  fossil 
in  a  quantity  of  chopped,  or  ground,  well  samples  taken  from  a  churn 
drill  hole.  A  red  shale  is  often  found  from  40  to  200  feet  above  the 
Herrin  coal.  This  red  bed  has  been  noted  in  Peoria  county  by  Dr. 
Udden;  in  Fulton,  Sangamon,  and  Clark  counties  by  T.  E.  Savage;  in 
LaSalle  county  by  Gilbert  Cady,  and  in  White,  Gallatin,  and  Saline 
counties  by  F.  W.  DeWolf.  It  occurs  high  up  in  many  well  records  in 
Crawford  and  Lawrence  counties  but  low  in  other  sections  of  the  State. 
The  Fusulina  limestone,  reel  shale,  and  top  of  the  No.  6  coal  are  the 
most  important  beds  in  the  McLeansboro  and  the  absence  of  any  two  of 
them  still  leaves  a  possible  means  of  determination  for  the  base  of  this 
division.  There  are  usually  300  feet  of  shale,  clay,  some  sand,  local  coal 
beds,  etc.,  between  the  Fusulina  limestone  and  the  Shoal  Creek  lime- 
stone. The  maximum  thickness  of  the  formation  in  southeastern.  Illinois 
is  about  1,000  feet. 

The  Carbondale  includes  the  rocks  from  the  Murphysboro  (No.  2) 
coal  to  the  top  of  the  Herrin  (No.  6)  coal.  Shale  constitutes  the  major 
part  of  the  division  with  much  micaceous  sandstone  in  the  basal  portion. 
There  are  several  beds  of  limestone  underlying  the  Herrin  coal.  The 
shales  are  soft  and  cavy  and  often  very  sandy,  so  closely  are  they  asso- 
ciated with  the  massive  Pottsville  sandstones  beneath.  The  sandstones 
are  sometimes  coarse  above  the  Murphysboro  coal.  This  coal  is  often- 
absent  and  a  thin  limestone  and  more  often  shale,  separates  the  Carbon- 
dale and  Pottsville.  There  is  a  good  bed  of  sand  usually  under  the 
Herrin  coal.  The  productive  oil-sand  north  of  Centralia  is  thought  to 
correspond  to  this  and  therefore  lies  in  the  Carbondale.  The  most  im- 
portant beds  of  this  division  are  the  Herrin  coal  at  the  top,  the  Murphys- 


blatchley]  GEOLOGY   OF    ILLINOIS.  29 

boro  coal  at  the  base  and  the  Harrisburg  (No.  5)  coal  between.  These 
coals  are  widely  distributed  and  give  good  opportunity  of  interpreting 
this  division.  The  formation  is  about  225  feet  thick  in  the  northern  part 
of  the  coal  area  of  Illinois,  and  300  to  450  feet  in  southern  counties. 

The  Casey  sands,  or  the  shallow  sands  of  Clark,  Coles,  Cumberland, 
and  Edgar  counties  and  the  400-foot  sands  of  the  Robinson  pool  in 
Crawford  county,  occur  well  up  in  the  Pennsylvanian.  They  are  inter- 
bedded  with  coals,  thin  limestones,  and  prevailing  shales.  They  have 
been  widely  drilled  along  the  La  Salle  anticline  and  have  been  found 
productive  of  oil  and  some  gas.  Their  shallowness  and  the  ease  of  drill- 
ing through  the  overlying  formations  has  caused  their  thorough  exploita- 
tion. These  sands  are  fairly  widespread  over  the  southern  and  central 
portions  of  Illinois  but  have  been  found  commercially  productive  in 
but  one  other  locality  beyond  the  La  Salle  fold.  The  original  oil  seep 
in  the  mine  north  of  Centralia,  which  gave  impetus  to  the  development 
of  the  Marion  county  oil  field,  is  from  a  sand  immediately  underlying 
the  Herein  coal.  _This  sand  was  found  productive  in  several  wells  north 
of  Centralia.  As  soon  as  the  position  of  the  Herrin  coal  is  definitely 
learned  in  the  main  oil  territory,  if  will  perhaps  be  possible  to  identify 
and  correlate  this  sand. 

The  Potts ville  sands  at  the  base  of  the  Pennsylvanian  have  been 
studied  in  Illinois  along  their  outcrop  by  David  White.  From  the  fossils 
they  are  believed  to  correspond  in  age  to  the  Pottsville  rocks  of  the 
Appalachian  region.  The  oil  and  gas  sand  of  Litchfield  apparently  be- 
longs in  the  Pottsville.  This  is  perhaps  the  only  instance  in  which  these 
formations  are  productive  of  oil  outside  the  Buchanan  sand  of  the  south- 
eastern Illinois  fields.  The  Pottsville  sandstones  of  the  central  and  south- 
ern portions  of  the  State,  especially  in  the  deeper  part  of  the  Illinois 
basin  and  over  the  LaSalle  anticline,  are  conspicuous  for  their  massive- 
ness.  Since  they  are  interbedded  with  shales,  however,  the  top  of  the 
formation  is  difficult  to  identify,  owing  to  the  merging  of  the  sands  with 
overlying  shaley  rocks.  The  correlations  in  this  report  were  based,  for 
the  most  part,  upon  the  top  of  the  thick  sand  immediately  underlying 
the  conspicuously  shaley  rocks.  These  sands  are  fairly  well  saturated 
with  salt  water  wherever  they  have  been  encountered.  They  commonly 
lack  conspicuous  limestone  strata,  thus  differing  distinctly  from  the 
underlying  Mississippian  rocks.  In  the  southern  part  of  the  State  the 
Pottsville  rocks  are  as  much  as  700  feet  thick. 

The  Mississippian  series  lying  in  the  Carboniferous,  next  below  the 
Pennsylvanian  ("Coal  Measures")  contains  important  oil  sands  whose 
exact  extent  is  not  accurately  known.  The  outcrops  of  the  Mississippian 
rocks  occur  around  the,  southern  and  western  borders  of  the  State,  and 
exposures  show  that  the  full  thickness  is  not  everywhere  present.  The 
thickest  development  occurs  in  the  southern  area.  It  wedges  out  to  the 
north  so  its  edge  is  overlapped  and  concealed  by  the  Pennsylvanian  rocks. 
The  Mississippian  oil  sands,  as  shown  by  the  table,  occur  in  the  upper  or 
Chester  members.  They  are  the  most  "productive  sano^s  ancl  nave  pro- 
duced most  of  the  oil  from  the  eastern  Illinois  fields. 

The  top  of  the  Chester  is  not  positively  recognized  in  drill  records. 
The  correlations  in  this  report  were  based  upon  the  limestone  immedi- 
ately underlying  the  massive  Pottsville  sandstone.     It  is  succeeded  by 


30  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 

other   limestones   interlain   with   strata   of   sandstones    and   red   shales. 
Weller  says  i1 

From  most  of  the  literature  on  the  subject  one  gains  the  impression  that 
the  Chester  is  dominantly  a  limestone  formation,  but  in  working  over  the 
area  occupied  by  the  beds  in  the  field,  one  is  impressed  with  the  fact  that 
it  is  in  a  large  part  sandstone.  Nowhere  in  that  part  of  Illinois  occupied 
by  these  beds,  is  the  limestone  element  in  the  formation  the  most  conspicuous 
feature,  except  along  the  Mississippi  river  bluffs  above  Chester,  from  that 
city  to  the  point  where  the  Cypress  sandstone  outcrop  begins.  It  is  prob- 
able that  where  the  limestone  has  its  greatest  development,  not  more  than 
one-third  of  the  total  thickness  is  calcareous,  and  over  a  large  part  of  the 
area  the  thickness  of  the  limestones  probably  does  not  exceed  one-fifth  of  the 
entire  thickness. 

The  best  region  in  which  to  study  the  succession  of  beds  in  the  Chester, 
is  in  the  Mississippi  river  bluffs  above  and  below  the  city  of  Chester.  This 
section  shows  an  alternation  of  chiefly  calcareous  and  arenaceous  formations, 
there  being  three  conspicuous  limestones  and  three  sandstones.  The  lime- 
stones are  frequently  interbedded  with  calcareous  shales,  and  the  sand- 
stones frequently  become  arenaceous  shales  or  at  times  clay  shales. 

The  lowest  member  of  the  "group,"  above  the  Cypress  sandstone,  is  a 
limestone  and  shale  formation  attaining  a  maximum  thickness  of  approx- 
imately 250  feet  at  and  above  Chester.  In  its  lower  portion  it  includes  con- 
siderable beds  of  calcareous  and  clay  shales,  a  bed  of  variegated  red  and 
blue  shale  being  commonly  present  near  the  base.  In  the  upper  part  of  this 
member  is  a  great  limestone  ledge  about  100  feet  in  thickness,  with  occa- 
sional thin  shaly  partings,  which  furnishes  the  quarry  rock  at  the  Southern 
Illinois  penitentiary,  at  Menard.  The  great  mass  of  the  fauna  of  the 
"Chester  group"  in  Illinois  has  been  described  from  this  lower,  calcareous 
member  of  the  formation  as  a  whole. 

The  second  member  of  the  "group"  is  a  sandstone  or  shale,  the  shale  be- 
ing most  conspicuous  in  the  more  northern  part  of  the  area,  while  to  the 
south  it  is  almost  wholly  a  sandstone  similar  to  the  Cypress  in  character, 
but  usually  thinner  bedded  and  not  infrequently  more  or  less  of  an  aren- 
aceous shale.  This  division  attains  a  thickness  of  about  80  feet.  The  third 
is  again  a  limestone  which  is  apparently  more  impure  than  most  of  the  beds 
of  the  lower  division.  It  is  much  less  fossiliferous  than  the  lower  division 
and  the  fossils  are  such  as  to  give  it  definite  faunal  characters  Which  can 
be  recognized  over  wide  areas.  Its  thickness  near  Chester  is  about  60  feet. 
The  fourth  member  is  again  a  sandstone  similar  to  the  earlier  sandstone 
beds,  and  attains  a  thickness  of  65  feet.  The  fifth  member  is  a  limestone 
similar  to  limestone  No.  2,  in  lithologic  characters,  and  is  usually  almost  or 
quite  unfossiliferous.     Its  thickness  is  about  35  feet. 

It  seems  to  be  altogether  probable  that  these  three  limestone  beds  of  the 
Chester  "group"  can  be  differentiated  and  mapped  throughout  the  faulted 
area  in  the  southern  part  of  the  State,  and  that  by  means  of  them  the  struct- 
ure can  be  worked  out  in  much  detail.  In  the  final  work  upon  these  beds  it 
will  probably  be  found  to  be  expedient  to  distinguish  each  of  these  six  mem- 
bers of  the  Chester  by  distinct  formation  names,  just  as  the  Cypress  sand- 
stone is  now  distinguished. 

Dr.  Weller  has  kindly  furnished  the  following  general  section  of  the 
Chester  rocks  from  the  exposures  along  the  Mississippi  bluffs  in  Kan- 
dolph  and  Monroe  counties,  Illinois: 


i  Weller,  Stuart,  The  Geological  Map  of  Illinois.    Bull.  III.  State  Geol.  Survey  No.  6, 1907. 


blatchley]  GEOLOGY    OF   ILLINOIS.  31 

■General  section  of  the  Chester   (above  the  Cypress  sandstone). 

Thickness 

Formations.                                                                             in  feet. 

Birdsville: 

Rockwood    sandstone     -L^u 

Limestone    (No.    3 )     20 

Arenaceous  shale  or  shaly  sandstone   47 

Sandstone     10 

Arenaceous  shale  or  shaly  sandstone    33 

Limestone    (No.   2 )    54 

Shale    42 

Limestone    (persistent  bed)     8 

Shale    (in    some    places    a    bed    of    sandstone    occurs    in    this    shale    of 

variable   thickness   from   0-20    feet) 36 

Limestone    4 

Shale    4 

Tribune: 

Limestone    (No.    1),    heavy   bedded    80 

Interval  of  uncertair   character,   lower  part  probably  shale   and  upper 

part    limestone    30 

Limestone    (fossils)     

Probably  shale — not  exposed    38 

Variegated  red  and  green  shales   15 

Not  exposed    5 

Limestone    (fossils)     20 

Shale,  thin  streak    ; 

Limestone     15 

Shale,    thin    strata     

Unknown    25 

Cypress    sandstone    134 

Total  depth  to  bottom  of  Cypress    769 

The  thinning  away  of  the  Chester  beds  to  the  north  causes  the 
absence  of  important  oil  and  gas  sands  in  that  part  of  the  State.  No 
Chester  has  been  found  present  west  of  a  line  from  Decatur  to  O'Fallon. 
Probably  there  is  little  Chester  north  of  a  line  between  Decatur  and 
Springfield. 

Pre-Chester  sands  of  the  Carboniferous  or  those  below  the  rocks  just 
described  are  not  present  in  the  main  fields.  These  rocks  have  been  very 
little  prospected  elsewhere  and  are  not  known  to  be  productive  in  other 
sections  of  the  State.  Kegardless  of  its  close  association  with  the 
Chester  proper,  its  wide  extent  and  porous  character,  the  Cypress  sand- 
stone is  not  looked  upon  as  holding  much  promise. 

The  Chester  group  is  limited  to  the  Tribune  formation  because  of 
upper  and  lower  erosion  periods  in  which  the  Birdsville  or  upper  division 
and  the  Cypress  or  lower  sandstone  member  have  entirely  disappeared. 

The  Ste.  Genevieve  limestone  underlies  the  Cypress  and  is  found  to 
be  highly  productive  of  oil  in  Lawrence  county.  This  bed  is  mostly  lime- 
stone but  conspicuously  oolitic  and  soft,  which  appears  to  be  a  recur- 
rence of  the  same  phase  of  the  lower  Salem  limestone.  Its  maximum 
thickness  in  the  oil  fields  is  85  feet  while  Weller  gives  100  feet  for  Mon- 
roe county.  The  McClosky  sand,  corresponds  to  the  Ste.  Genevieve. 
Below  that,  in  the  Carboniferous,  are  no  known  beds  that  are  either 
encouraging  or  discouraging  as  possible  sources  of  oil.  A  very  recent 
report,  however,  describes  the  finding,  of  oil  300  feet  below  the  top  of 
the  St.  Louis  limestone  on  the  Hardacre  farm,  K  E.  %  Sec.  10,  T.  3  N., 
E.  12  W.,  Lawrence  township,  Lawrence  county.  This  may  indicate  an 
oil  horizon  at  this  position  in  the  series.  Petroleum  has  also  been  found 
in  the  geode  bed  of  the  Keokuk.  This  is  not  believed,  however,  to  be 
especially  significant. 

The  Silurian  includes  the  Niagara  limestone  formation,  which  in 
northern  Illinois  is  dolomitic,  and  locally  contains  bituminous  deposits. 
It  offers  some  slight  chance  of  oil  production. 


32  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 

The  Ordovician  system  includes  the  Galena-Kimmswick  limestone, 
along  with  others  of  little  importance  in  this  connection.  Over  it  lie 
the  Richmoncl-Maquoketa  shales  which,  in  the  northwest  counties,  are 
rich  in  disseminated  oil.  The  Galena-Kimmswick  is  known  to  be  300- 
400  feet  thick  in  the  north;  250  feet  thick  in  Calhoun  and  Jersey 
counties;  at  least  100  feet  in  southern  Illinois.  It  doubtless  underlies 
the  younger  rocks  of  the  Illinois  basin. 

Structure. 

Throughout  the  central  portion  of  Illinois  there  is  a  spoon-shaped 
basin  with  its  long  axis  extending  from  the  north  line  of  Stephenson 
county  past  La  Salle,  Lovington,  and  continuing  to  the  southwest  county 
of  Indiana.  The  deepest  part  of  the  basin  lies  in  the  vicinity  of  Wayne, 
Hamilton,  Edwards,  and  White  counties,  where  the  rocks  are  compara- 
tively fiat.  Towards  this  basin,  with  local  exceptions,  all  the  rocks  of 
Illinois  and  of  western  Indiana  dip  gently.  The  sides  of  the  "spoon" 
show  some  minor  longitudinal  folds.  The  most  important  is  the  LaSalle 
anticline  (See  Plate  IB)  which  runs  from  Freeport  to  a  point  just  east 
of  LaSalle,  and  continues  in  a  southeasterly  direction  through  the  oil 
field  and  into  Indiana.  From  western  Illinois  the  rocks  dip  gently  east- 
ward until  the  Duquoin  anticline  is  reached  but  then  dip  much  more  rap- 
idly to  the  axis.  They  rise  from  this  line  to  the  LaSalle  anticline,  decline 
gentry,  and  then  rise  again  into  Indiana.  The  dips  of  the  southern  rocks 
into  the  basin  are  locally  100  feet  or  more  to  the  mile.  The  anticlines 
and  other  minor  irregularities  influence  the  accumulation  of  oil  and  gas 
as  explained  in  a  previous  discussion,  and,  therefore,  are  of  special  im- 
portance. They  become  less  conspicuous  towards  northern  Illinois ;  conse- 
quently that  part  of  the  State  does  not  offer  as  promising  structural 
features,  for 'the  accumulation  of  oil  as  the  southern  part  and  it  more- 
over, entirely  lacks  the  Pennsylvanian  and  Mississippian  oil  sands.  Oil 
if  present  must  be  found  in  the  older  formations. 

STEATIGBAPHY  OF  CRAWFORD  AND  LAWRENCE 
COUNTIES. 

General  Statement. 

The  stratigraphy  of  Crawford  and  Lawrence  counties  is  revealed  by 
the  study  of  two  sets  of  columnar  sections  comprising  the  most  repre- 
sentative borings  in  the  two  counties.  Three  of  the  records,  2,  5,  and  10 
of  the  Lawrence  county  and  all  of  the  logs  of  the  Crawford  county  sec- 
tions are  precise  studies  of  well  samples  collected  by  the  writer  and 
examined  by  Dr.  J.  A.  Udden. 

Crawford  County. 

All  the  penetrated  rocks  in  the  producing  areas  of  Crawford  county 
belong  to  the  Pennsylvanian  series.  These  rocks  are  overlain  by  a  vary- 
ing thickness  of  drift..  The  Pennsylvanian  series  are  represented  by 
about  480  feet  of  the  McLeansboro,  300  feet  of  the  Carbondale,  and 
about  100  feet  of  the  Pottsville  formations..    The  rocks  are  all  of  sedi- 


blatchley]  CRAWFORD   COUNTY   LOGS.  33 

mentary  origin   being  principally   shales   with  variable   intergradations 

of  sandstones,  limestones  and  coal.     The  columnar  section  of  Crawford 

county  is  made  up  of  logs  from  several  localities,  several  of  which  are 

outside  the  area  covered  by  this  report.    They  are  plotted  in  order  from 
Mi--———  in 

a 

.11 
e- 
le 


405 

410 

410 

415 

415 

420 

~^~,w.«...  &ia.y  nLni.  snaie,  nne  texture  with  many  fragments  of  coal 

Gray   shale   of   fine   texture,   fossil   fragments,   bits 

Shale,    sandy,   micaceous   greenish   gray,   with   leaf   imprints 

Shale,    sandy,    micaceous   and     greenish     gray     with     small     black 

fragments  of  vegetation    420  425 

—3  G 


32  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 

The  Ordovician  system  includes  the  Galena-Kimmswick  limestone, 
along  with  others  of  little  importance  in  this  connection.  Over  it  lie 
the  Richmoncl-Maquoketa  shales  which,  in  the  northwest  counties,  are 
rich  in  disseminated  oil.     The  Galena-Kimmswick  is  known  to  be  300- 

400     fpp+    ±kials     in     +Lr>    T.^-n+T,  •     OKA     4?-~i-    J-i.:  _i_     •-      n    n  ^      ^ 

coun 
the  3 


Tr 
basin 
comrl 
of  In 
Ham 
tivel} 
Illinc 
show 
antic! 
of  U 
field, 
ward 
idly  t 
genth 
into  t 
and  o 
as  ex] 
porta: 
quent 
featui 
over, 
if  pre 


Th€ 

the  st 
sentat 
of  the 
tions 
exami: 


All  __■__       __  J 

belong  to  the  Pennsylvanian  series.  These  rocks  are  overlain  by  a  vary- 
ing thickness  of  drift,.  The  Pennsylvanian  series  are  represented  by 
about  480  feet  of  the  McLeansboro,  300  feet  of  the  Carbondale,  and 
about  100  feet  of  the  Pottsville  formations..    The  rocks  are  all  of  sedi- 


blatchley]  CRAWFORD   COUNTY   LOGS.  33 

mentary  origin  being  principally  shales  with  variable  intergradations 
of  sandstones,  limestones  and  coal.  The  columnar  section  of  Crawford 
county  is  made  up  of  logs  from  several  localities,  several  of  which  are 
outside  the  area  covered  by  this  report.  They  are  plotted  in  order  from 
south  to  north  in  Plate  II.  The  top  of  the  limestone  over  the  Herrin 
coal,  which  may  be  called  the  "Fusulina"  limestone  for  the  lack  of  a 
geographical  name,  is  used  as  a  key  line  for  the  columnar  section.  All 
the  records  are  plotted  with  respect  to  this  line  and  are  presented  here- 
with, corresponding  by  number  to  those  printed  on  Plate  II.  All  of  the 
following  logs  were  compiled  by  Dr.  J.  A.  Udden  from  a  detailed  ex- 
amination of  well  samples  saved  by  the  Ohio  Oil  Company. 

LOGS. 

No.   l.—M.  Shiltz,  No.  7. 

Location— SE.  ^4  sec.  7,  T.  7  N.,  R.  14  W.,  Oblong  Township. 
Elevation — 485  feet. 

Unknown    

Light  gray  micaceous  sandstone  or  sandy  shale.  The  laminae 
are  from  one-twentieth  to  one-eighth  of  an  inch  in  thickness .  .  . 

Gray  micaceous  shaly  sandstone,  with  carbonaceous  foliations 
showing  leaf  fragments  and  needle-like  impressions.  Biotite 
scales    noted    

Gray  micaceous  shaly  sandstone  and  black  carbonaceous  shale... 

Gray  micaceous  shaly  sandstone,   with  carbonaceous   foliations.  .  . 

Gray  calcareous  limestone,  partly  organic  fragmental,  apparently 
concretionary.  A  fragment  of  a  black  silicified  piece  of  a 
fern  stem  noted   

Light   gray   sandy   shale,   micaceous    

Gray  sandstone,  fine  in  texture,   and  with  a   calcareous  matrix.  .  . 

Light    gray,    sandy    shale    

Light  gray  sandy  and  micaceous  shale  and  some  calcareous  con- 
cretionary material    

Dark   micaceous   shale   and   micaceous   gray   sandstone 

Gray,    stony    shale 

Black  fissile   shale,    "miners   slate."   and   greenish   fire   clay 

Gray  sandy  shale  and  black   shale    

Greenish    gray   shale    of   fine   texture    

Light   gray   shaly   sandstone   and    shale,    biotitic 

Light  gray  sandy  and  micaceous  shale,  with  some  dark  and  soft 
marly    material     

Gray    sandy    shale    

Dark    gray    sandy   shale    

Dark  gray  sandy  and  micaceous,   stonv   shale    

Dark  gray  stony  shale  and  green  fire  clay    

Dark  gray  shale  of  fine  texture    

Dark  shale,  with  impressions  of  narrow  leaf-like  forms  of  vegeta- 
tion and  of  fragments  of  thin  shells 

"Miners'   slate,"   black,   and   some   coaly   shale    

Gray    sandstone,    moderately   coarse    

Light  gray  sandy  shale,  with  layers  of  shaly  sandstone,  which 
contains  spherules  of  brown  carbonate   of  iron 

Gray    calcareous    limestone     

Gray  limestone  and  some  black  shale.  Chetetes  milleporaceus 
noted     

Micaceous  gray  sandy  shale  or  sandstone  with  some  concre- 
tionary   limestone    

Gray  micaceous  sandstone  and  sandy  shale 

Gray  soft  shaly  sandstone.     Some  fragments  have  a  brownish  tint 

Gray   shale   of   fine   texture    

Gray  sandy  shale,    light 

Micaceous  and  sandy  stiff  shale,  light  gray,  with  narrow  impres- 
sions, carbonaceous,  of  small  leaves  and  bits  of  brown  tests  of 
crustaceons.     Many  fragments  of  coal    

Medium  gray  stiff  shale,  fine  texture  with  manv  fragments  of  coal 

Gray   shale   of   fine   texture,   fossil   fragments,    bits 

bhale,    sandy,   micaceous   greenish   grav.    with    leaf   imprints 

bhale,    sandy,    micaceous    and     greenish     grav     with     small     black 

fragments  of  vegetation 420  425 

—3  G 


Depth  in 

feet. 

From 

To 

0 

185 

185 

190 

190 

200 

200 

205 

205 

210 

210 

215 

215 

220 

220 

230 

230 

250 

250 

255 

2*55 

260 

260 

265 

265 

270 

270 

2  75 

275 

280 

280 

285 

28n  • 

290 

290 

295 

295 

300 

300 

320 

320 

325 

325 

335 

335 

340 

340 

345 

345 

350 

350 

355 

355 

360 

360 

365 

365 

370 

370 

380 

380 

390 

390 

395 

395 

400 

400 

405 

405 

410 

410 

415 

415 

420 

Depth  in 

feet. 

From 

To 

425 

440 

440 

445 

445 

450 

450 

455 

455 

470 

470 

475 

475 

480 

34  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE   COUNTIES,    [bull.  no.  22 

Logs — Continued. 


Sandstone,    fine   in   texture,   micaceous,    shaly   light   gray 

Gray  shale  of  fine  texture,  greenish,  only  very  slightly  micaceous 

Sandy   shale,   gray,   micaceous,   with   bits  of  vegetation 

Light  gray   shale,   stony    

Shale,    greenish    gray,   micaceous    

Dark   greenish   gray    shale,    of   fine,    even   texture 

Coal  and  fine  gray   shale  or  fire   clay    

Limestone,  some  dark  and  compact  with  very  slow  effervescense, 
some  light,  calcareous,  crystalline  cleavage  like  that  in  crinoid 
stems.  Also  some  limestone  and  shale,  with  small  spherules  of 
clay  iron   stone,   magnetic  after   fusion,    y%-x/%   mm.   in   diameter. 

Wood   in    coaly   pyrite *  480  485 

Shaly   sandstone   of   light   gray    color    485  495 

Dark  gray  stony  micaceous  shale    495  500 

Gray    sandstone    and    shale    500  505 

Gray   shale,    stiff,    of   fine    texture 505  510 

Dark    gray    micaceous    shale    510  515 

Gray    dark    shale,    stiff,    micaceous    515  520 

Gray  limestone  and  coal,  limestone  is  organic  fragmental.     Crinoid 

joints    noted    520  525 

Coal   and   some    gray   fire   clay    525  530 

Gray  sandstone  with  a  little  micaceous   shale    530  540 

Gray   sandstone   with    sandy   shale    540  545 

Gray   sandstone,    fine    545  550 

Gray  micaceous   stony,    (sandy)    shale    550  570 

Gray   shaly   fire    clay   or   shale    570  575 

Dark  shale  and  a  little  coal.     Shale,   fine  and  carbonaceous 575  580 

Dark  shale,   coal  and  fire  clay    580  585 

Black  limestone  (almost),  effervescing  slowly,  with  imbedded 
organic  fragments  and  pyrites,  yellow.  Green  grains  or  fillings 
in    limestone,    crinoid    stems,    fragments    of    shells,    and    spines, 

fusulina    fossils     585  590 

Dark  gray  stiff  micaceous   shale    590  595 

Gray  micaceous  shaly  sandstone   and  shale    595  600 

Shaly    sandstone,    gray,    micaceous     600  605 

Dark  calcareous  limestone,  with  Athyris,  crinoid  stems,  spines,  in 

copious  small  fragments,  and  coal  in  coarse  and  fine  fragments  605  610 

Black  shale,   gray  shale,   fire  clay  and  coal    610  615 

Gray   sandstone    and    black    shale    615  620 

Gray    sandy    shale     620  625 

Sandstone,    light    gray,    of    fine    texture    thinly    laminated,     some 

yellow    concretionary    material     625  630 

Gray   shaly   sandstone,    micaceous    635  640 

Gray   sandy   shale    and   fire    clay    640  645 

Gray    sandy    shale     645  650 

Gray  shale   of  fine  texture    650  660 

Gray   sandy   shale   with    straight   laminations    660  665 

Black  shale,  with  gray  blotches,  laminated,   "Miners'   slate" 665  670 

Black  shale   and   dark  gray  shale    670  675 

Light  greenish  gray  shale  of  fine  texture    675  685 

Black  shale,  almost  slaty   685  690 

Black   stiff   shale  of   fine   texture    690  695 

Dark   gray   shale    695  700 

Gray    sandy    shale     700  705 

Gray  stiff  shale,  and  some  earthy  shale    705  710 

Dark  gray  earthy  shale  and  light  gray  sandstone    710  715 

Dark    gray   laminated    shale    715  725 

Dark    gray,    laminated,    micaceous    shale,    with   imprints   of   leaves 

and    bits   of   vegetation    725  730 

Gray    shale,    sandy    and    micaceous,    with    imprints    of    fragments 

of    leaves    730  735 

Dark,    very   dark    shale,    micaceous    735  740 

Black   shale,    short    "miner's   slate"    740  745 

Black   shale,   short   "miner's   slate,    with   pyrites    745  750 

Gray   sandstone   with    some    coal    750  755 

Sandstone,   shale,  laminated,   dark  gray   755  760 

Dark    gray    shale 760  765 

Shale,   dark  gray,    some   dark  fire  clay,   coal    765  770 

Coal,    hardly   anything   else,    large    sample    770  775 

Light   gray   sandy  fire   clay  and   coal    775  780 

Light  gray  micaceous  pyritiferous  sandstone  and  some  dark  shale  780  785 

Light   gray  micaceous   sandstone    785  790 

Micaceous   light   gray   sandstone    (and    shale) 790  795 

Sandy  gray  shale  and  fire  clay,  dark,  and  showing  slickensides.  .  795  800 

Dark  gray  shale,  fine  in  texture,  with  some  slickensided  pieces...  800  805 

Black    "miners'    slate"     805  810 

Black  coaly  shale,  with  a  light  gray  rock  composed  of  clay  and  con- 
taining small  spherules  of  clay  iron  stone  %-%  mm.  in  diameter  810  815 


?A 


Sa 
Gr 
Sa 
Li? 
Sh 
Da 
Co 
Lii 


Sh. 

Da 

Gr 

Gr, 

Da 

Gr 

Gr 
J 

Co; 

Gr; 

Gr; 

Gr; 

Gn 

Gr; 

Da 

Da 

Bh 
c 
i 

D.' 

Gn 
Shi 
Da 

c 

Bl£ 

Gn 
Gn 
Sai 

Gn 
Gn 
Gn 
Gn 
Gn 
Bla 
Bla 
Lig 
Bla 
Bla 
Dai 
Gn 
Gn 
Dai 
Dai 
Dai 

a 
Grs 

o 
Dai 
Bla 
Bla 
Gra 
Sar, 
Dai 
Sha 
Coa 
Lig 
Lig 
Lig 
Mic 
San 
Dai 
Bla 
Bla 


BLATCHLET] 


CRAWFORD   COUNTY   LOGS. 


35 


Logs — Continued. 


Dark  gray  shale  with  some  fine  small  flakes  of  mica 

Coal  and  some  dark  shale,  with  fragments  of  brown  clay  iron  stone 

Fire   clay,   shale,   dark   and   light   gray   sandstone 

Dark  gray  shale  and  shaly  light  gray  sandstone    

Black   shale,   coal   and  fire   clay    

Gray  sandy  shale   and  black  shale,   some   coal    

Gray  sandy  shale,   black   shale,   some   coal    

Black  and  gray  shale,    laminated    (?)    

Dark  gray  shale,  micaceous,  and  sandy  light  gray  shale 

Black   shale   and  gray  shale,   micaceous,   imprints   of  leaves 

Gray  and  black  shale,  some  of  the  black  shale  with  thin  laminae 
of    coal     

Gray  micaceous   and  sandy  shale   and  shaly   sandstone 

Black  coal  shale  ("miners'  slate")  some  impure  coal  and  some 
fire    clay    

Dark  gray  shale,   stiff 

Some  gray  shale,  some  shaly  sandstone,  seme  cloddy  limestone 
with  crinoid  stems  and  other  fossils  in  fragments.  Much  of  the 
sample  is  a  stony,  sandy  fireclay,  in  which  are  imbedded  spher- 
ules of  clay  iron  stone  %-%mm.  in  diameter.  On  grinding  and 
polishing  some  fragments  containing  these  spherules  a  center  of 
pyrite  was  seen  in  some  of  the  spherules.  The  imbedded 
spherules  lie  quite  close  together,  giving  the  appearance  of 
oolitic    rock 

Gray  micaceous  sandy  shale  and  fire  clay 

Gray  shaly  micaceous  sandstone  or  sandy  shale 

Gray    shale    micaceous    sandstone 

Gray  sandstone,  foliated,  with  carbonaceous  black  foliations 

Yellowish  sandstone,  ground  up,  floats  on  water 

Gray  sand,  less  oily.      %-%  mm. 


Depth  in 

feet. 

From 

To 

815 

820 

820 

825 

825 

830 

830 

835 

835 

840 

840 

845 

845 

850 

850 

855 

855 

860 

860 

865 

865 

870 

870 

875 

875 

880 

880 

885 

885 

890 

890 

895 

895 

905 

905 

910 

910 

920 

920 

925 

No.  2. — 0.  F.  Edwards,  No.  15. 


Location — SE.  %  sec.  7,  Oblong  Township. 
Elevation— 485  feet. 


Loess  or  silt,  with  some  sand 

Boulder    clay,    thoroughly    leached 

Yellow   boulder  clay,    calcareous 

Yellowish  gray  calcareous  boulder  clay  with  limestone  pebbles... 

Sand  and   gravel  washed  from  boulder  clay 

Gray   boulder   clay 

Sand  and  gravel,  washed  from  boulder  clay 

Mostly  sandstone,  fairly  coarse,  with  some  limestone  with  frag- 
ments of  fossils,  probably  Productus  semirecticulatus,  Retzia, 
Rhomhopora  lepidodendroides,  Fislulipora,  Tubipora,  and  joints 
of    crinoid    stems 

Sandstone,    gray,    micaceous,    friable 

Gray  shale,  slightly  micaceous,  of  comparatively  loose  consistency 

"Dirt  bed"  material,  dark  crumbling  silt  clay,  with  some  coal .... 

Impure  fire  clay  and  shale,  much  coal,  and  concretions  of  lime 
and   of   carbonate   of   iron 

Dark    shale 

Gray    shale,    micaceous 

Gray  shale  and  marly  material.  The  latter  contained  the  pygidium 
of  a  small  trilohite,  fragments  of  bryozoa,  and  joints  of  crinoid 
stems     

Almost  black  shale,  containing  small  ostracods,  one-thirtieth  of 
an  inch  in  length  and  an  impression  of  some  smooth  flat  objects, 
having  the  shape  of  an  equilateral  triangle  with  perfectly 
straight  sides  measuring  a  sixth  of  an  inch 

Black  shale  with  impressions  of  fucoidal  bands  a  tenth  of  an 
inch  in  width.  Part  of  sample  a  dark  limestone  with  crinoid 
stems,  a  small  pentagonal  crinoid  plate,  and  a  small  brachiopod 
(Ambocoeia    umbonata?) 

Dark  limestone,  of  characteristic  appearance  of  a  "clod"  lime- 
stone (i.  e..  small  limestone  overlying  a  coal),  clay,  fissile,  shale 
and  coal.  The  limestone  has  the  same  fossils  as  in  the  previous 
number     

Dark  limestone  as  above,  with  irregularly  bending  Ammodiscus 
tubes  about  one-fifth  inch  in  diameter,  also  coal  and  some  fire 
clay.  The  coal  probably  lies  at  a  depth  of  about  125  feet  and 
is  underlaid  by  the   fire   clay 

Gray    micaceous    sandstone 

Micaceous  shaly  sandstone   and  sandy  shale 


Depth  in 

feet. 

From 

To 

0 

5 

5 

15 

15 

20 

20 

25 

25 

40 

40 

45 

45 

50 

50 

55 

55 

65 

65 

85 

85 

90 

90 

95 

95 

100 

100 

105 

105 


110 


115 


120 


110 


115 


120 


125 


25 

130 

30 

140 

40 

145 

Depth  in 
From 

feet. 
To 

145 
150 
155 
160 

150 
155 
160 
165 

165 
170 
175 

170 
175 
180 

180 
185 
190 
195 

185 
190 
195 
200 

200 
210 
215 

210 
215 
220 

220 
225 
230 

225 
230 
235 

36  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE   COUNTIES,    [bull.  no.  22 

Logs — Continued. 


Micaceous    shaly    sandstone 

Micaceous  shaly  sandstone  and  sandy  shale 

Coal,   some  "clod"  and  some  shale 

Gray    micaceous    sandstone 

Gray  micaceous  sandstone  with  one  large  piece  of  coal  and  one 
large  piece  of  black  shale,  containing  fragments  of  some  thin 
shells,   probably  a   Lingula 

Gray  sandstone,   with  some  calcareous   rock 

Shaly   micaceous   gray   sandstone 

Shaly  micaceous  gray  sandstone,  with  some  small  fragments  of 
a    calcareous    rock 

Dark  gray  sandy  shale  with  large  flakes  of  mica 

Dark   gray    micaceous    shale 

Gray  micaceous  shale,  with   shreds  of  vegetation 

Limestone,  compact,  yellowish  white  and  dark  gray,  containing 
crinoid  stems  and  fragments  of  other  unidentified  fossils.  Splits 
into  thin  fragments,  and  has  a  sort  of  waxy  lustre 

Gray    shale,    somewhat    micaceous 

Fire  clay,   shale,   and  sandstone 

Mostly  sandstone  having  a  calcareous  matrix  and  a  few  imbedded 
organic    calcareous    fragments 

Sandy  shale  or  shaly  sandstone,  with  some  black  mica 

Gray    sandstone 

Gray  sandstone,  laminated,  with  thin  layers  of  carbonaceous 
material    235  240 

Dark  gray  sandstone,  laminated,  micaceous,  with  thin  carbonace- 
ous foliations,  and  with  a  calcareous  cement.... 240  245 

Sandstone,  dark  gray,  shaly,  biotitic.  Some  fragments  show  yel- 
low specks  of  presumably  concretionary  iron  carbonate,  other 
fragments  are  closely  studded  with  minute  grains  of  pyrite.... 

Some  sandstone  like  the  previous,   dark  shale   and  fire   clay 

Dark   shale    and   sandstone,    both    biotitic 

Black  shale  and  some  fragments  of  a  coarse  shell  breccia,  con- 
taining   crinoid    stems 

Gray    sandstone 

Gray  sandstone,  with  a  brown,  slowly  effervescing  sandstone 

Gray  sandstone,  with  a  brown,  slowly  effervescing  sandstone,  with 
more  of  the  brown  rock,  which  seems  to  have  a  concretionary 
(oolitic)  structure  and  consists  of  mainly  carbonate  of  iron  with 
some    calcareous    grains 

Gray    sandstone,    micaceous 

Gray  sandstone,   micaceous,   with   some   shaly   sandstone 

Gray    sandstone,    micaceous 

Gray   shale 

Gray  shale  with  small  ostracods,  and  a  spiral  Ammodiscus 

Gray  shale,  with  narrow,  ribbon-shaped  impressions  of  vegetation, 
ostracods    and    a    spiral    Ammodiscus 

Gray  sandy  shale   and  micaceous   sandstone 

Micaceous   sandstone  and  coarse  gray  shale 

Coarse    sandstone 

Sandstone,    with    yellow    grains    (concretionary)    of    carbonate    of 

iron,  larger  than  the  sand  grains 340  345 

Gray   shale   with    some   very   compact   fragment?   of   carbonate    of 

lime    concretions 345  350 

Faintly   yellowish    gray    limestone,    splitting    into   thin    chips,    with 

many   unrecognizable   fragments   of   organic   origin 350  360 

Limestone,  like  the  preceding,  with  a  brachiopod  shell  fragment, 
a  Zaphrentis,  and  joints  of  crinoid  stems.  Also  some  dark  gray 
shale     •. 

Greenish  gray  shale 

Gray   micaceous    sandstone    and    shale 

Gray  shale  of  fine  texture 

Bluish   gray   sandstone 

Shale,  mostly  dark  gray,  and  of  fine  texture 

Sandstone    and    sandy    shale 

Micaceous   sandstone   and   shale 

Gray   silty   shale 

Dark  gray  shale 

Gray  sandstone  and  shale 

Gray  shale  and  some  impure  coal 

Micaceous  gray  shale,  with  fragments  of  concretions  of  carbonate 
of    iron 

Gray   shale 

Gray  shale  or  fire  clay 

Gray  shale,   stony  and   dark,   micaceous 

Some  gray  shale  like  the  above.  But  mostly  a  dark,  dirty  yellow 
clay,  too  oily  to  mix  with  water,  giving  off  gas  and  oil  when 
heated  and  loosing  much  of  its  weight,  probably  30  or  40 
per    cent 455  46° 


245 

250 

250 

255 

255 

260 

260 

270 

270 

275 

275 

280 

280 

285 

285 

295 

295 

300 

300 

310 

310 

315 

315 

320 

320 

325 

325 

330 

330 

335 

335 

340 

360 

365 

365 

370 

370 

385 

385 

395 

395 

400 

400 

405 

405 

410 

410 

415 

415 

420 

420 

425 

425 

430 

430 

435 

435 

440 

440 

445 

445 

450 

450 

455 

From 

To 

460 

465 

465 

470 

470 

475 

475 

480 

480 

485 

485 

490 

490 

500 

500 

505 

505 

510 

510 

515 

515 

520 

520 

525 

525 

535 

535 

540 

540 

545 

545 

550 

550 

555 

blatchlet]  CRAWFORD    COUNTY   LOGS.  37 

Logs — Continued. 

Depth  in  feet. 

Like  the  previous,   with  much   coal    

Sandstone,  gray,  micaceous,  and  some  pieces  of  a  black  limestone, 
containing    fragments    of    fossils     

Oily   clay,   with  coal   and  gray   stony  shale,   some   pyrite 

Like  the  previous,  with  much  coal  and  some  fossiliferous  limestone 

Sandstone,  with  some  yellow  limestone  containing  organic  frag- 
ments      

Gray  shale  and  some  sandstone    

Dark  gray   shale    

Dark  gray  shale  with  a  small  Ammodiscus  and  some  narrow 
fucoid   markings    

Gray  limestone  with  imbedded  yellow  fragments  of  fossils  with 
some  black  shale  and  coal    

Mostly  fire  clay  and  coal    

Sandstone,  some  coarse,  some  thinly  laminated   

Sandstone,    comparatively   coarse    

Sandstone  of  average  texture   

Dark   arenaceous   shale    , 

Shaly  sandstone,   black   shale   and  coal    

Some  coal,  fire  clay,  and  dark  sandy  shale   

Mostly  coal,  some  black  shale  and  fire  clay   

Gray  sandstone,  with  a  compact  yellowish  gray  limestone  break- 
ing frequently  into  rectangular  fragments,  and  probably  of  con- 
cretionary   origin     555  560 

Dark  shale  and  sandy  gray  shale  with  fragments  of  concretions 
of   carbonate    of   iron    

Gray   shaiy   sandstone    

Dark  "cloddy"  shale  and  coal  with  some  sandstone 

Coal,  stony  fire  clay  and  sandy  shale    

Gray  sandy  shale    

Shaly    sandstone     

Shaly  sandstone,  greenish  sandy  shale,  coal  and  concretionary 
carbonate   of   iron 

Gray  shale    

Dark   gray   shale,   hard    

Dark  gray  shale  with  a  fine  textured  and  compact  limestone,  in 
part  gray,   in   part  yellow,   apparently  concretionary 

Gray  shale,  with  concretionary  limestone  like  that  in  the  above.  . 

Gray  sandstone  and  some  black  shale    

Gray  fine-grained  sandstone,  with  some  black  coaly  shale 

Like  the  preceding,  but  less  shale   

Gray  shale  and  black  shale    

Gray   shale    

Black  micaceous  shale  and  gray  shale  with  concretionary  material 

Black  micaceous  shale  with  concretionary  material 

Gray  and  black  shale  and  coal    

Coal  and  gray  shale   

Gray  shaly  and  micaceous  sandstone  with  much  carbonaceous 
material,  and  with  imprints  of  vegetation  abundant  in  some 
fragments     685  690 

Dark  gray  sandstone  of  fine  texture  with  thin  layers  of  car- 
bonaceous   material    

Dark  gray  micaceous  shale  with  imprints  of  fern  leaves 

Dark   gray   shale,   micaceous    

Dark  gray  shale,  micaceous,   stony    

Black    shale,    hard    

Black   shale    

Black  shale,  with  "clod"  limestone  containing  a  crinoid  stem 
and    some    coal     

Gray  micaceous  sandstone,  comparatively  coarse  in  texture 

Gray   sandstone    

Shale,   almost  black    

Black  shale  and  coal    

Black  shale  and  fragments  of  "clod"  limestone,  coal  and  fire  clay 

Gray  micaceous  sandstone,  with  brown  concretionary  material .... 

Gray  sandstone  and  black  shale    

Gray   shale   and   some    sandstone    

Gray  sandstone  and  shale,  with  much  brown  concretionary 
material     

Like  the  preceding,  with  some  calcareous  material   

Gray  shale,  and  some  fire  clay  with  thin  carbonaceous  flakes 
imbedded    

Dark  gray  shale,  micaceous    

Shale,   almost  black    

Black  and  gray  shale,  some  "clod"  limestone,  some  fire  clay  and 
some  concretionary  carbonate  of  lime    

Black  clayey  shale,  some  coaly  shale,  some  brown  and  soft  con- 
cretionary   material     

Da/k  bluish   shale  and  some   sandstone    


560 

565 

565 

570 

570 

575 

575 

580 

580 

585 

585 

590 

590 

600 

600 

605 

605 

630 

630 

635 

635 

640 

640 

645 

645 

650 

650 

655 

655 

660 

660 

665 

665 

670 

670 

675 

675 

680 

680 

685 

690 

695 

695 

700 

700 

705 

705 

725 

725 

730 

730* 

735 

735 

740 

740 

745 

745 

750 

750 

755 

755 

760 

760 

770 

770 

775 

775 

780 

780 

785 

785 

790 

790 

795 

795 

800 

800 

810 

810 

820 

820 

825 

825 

830 

830 

835 

38  OIL  FIELDS  OF  CRAWFOKD  AND  LAWRENCE   COUNTIES,   [bull.  no.  22 

Logs — Continued. 

Depth  in  feet. 
From  To 

"Clod"   limestone,   dark  and  black  shale,   coal,   and  greenish  shaly 

fireclay    835  840 

Bluish  gray  shaly  fire  clay  and  black  shale   840  845 

Gray  fire  clay  and  some  coal    845  X50 

Black  shale,   gray  shale  and   sandstone    850  855 

Gray  shale  and  shaly  sandstone   855  860 

Black  shale  and  coal,  with  some  concretionary  carbonate  of  iron.  .  860  875 

Black   shale   and   gray   shale   with   much    concretionary   carbonate 

of  iron  and  some  coal    875  880 

Dark  gray  shale  with  concretionary  carbonate  of  iron 880  885 

Dark  gray  shale,  with  much  concretionary  carbonate  of  iron 885  390 

Black  micaceous  shale    890  £95 

Black  shale  slightly  micaceous    895  900 

Mostly  black  shale,  with  some  concretionary  material    900  905 

Thinly  laminated  shale  with  alternate  layers  light  and  dark 905  910 

Dark  gray,   stiff  shale    910  915 

Dark  gray  shale,  laminated,  with  alternate  layers  of  light,  sandy, 

dark   and   finer  texture    915  920 

Laminated  shale,  sandy  laminae,   about  four,   in  a  thickness  of  a 

sixteenth  of  an  inch 920  925 

Like  the  previous,  but  with  sandy  laminae,  thicker   925  940 

Coaly  black  shale  and  gray  shaly  sandstone,  both  micaceous 940  945 

Black  shale,  greenish  gray  shale,  and  sandstone 945  950 

Incoherent  gray  sand,   some   70   per  cent  of  the  grains  measuring 

from    one-eighth    to    one-fourth    of    an    millimeter    in    diameter, 

some  20  per  cent  measuring  less  than  one-eighth  mm.  and  only 

a  few  per  cent  measuring  more  than  one-fourth  of  a  mm.     The 

sand    floats    on    water 950  955 

Black  shale    955  960 

Black  shale,   brownish   concretionary  carbonate   of   iron   and   some 

sand     •. 960  965 

Gray,    faintly    brownish    sand   which    floats    on    water,    with    some 

coherent  lumps  which  emit  oil  when  heated   965  970 

Thinly  laminated  shaly  sandstone,   alternate  laminae   of  dark  and 

lisrht   material.      Laminae    mostly   about    one-half    millimeter    in 

diameter.     Slightly  effervescent  with  acid    970  975 

Like  the  preceding,  but  more  shaly  and  lamination  less  frequently 

to  be   seen 975  980 

Dark  stony  shale,  with  thin  layers  of  alternating  light   and   dark 

material,  with  some  concretionary  brownish  carbonate  of  iron.  .  .  980  985 

Sandy    laminated    shale    or    shaly    sandstone,    layers    bending    and 

curving     985  990 

Note — Dr.  Udden  adds  the  following  statement  to  the  above  log: 
"The  limestone  at  360  feet  is  probably  correlative  with  a  limestone 
horizon  which  occurs  at  about  160  feet  above  Coal  No.  6,  in  the  Belle- 
ville region.  The  limestone  at  200  feet  is  most  likely  an  equivalent  to 
the  Carlinville  limestone  about  150  feet  higher  in  the  section.  Coal 
No.  6  is  believed  to  be  the  coal  at  510  feet.  The  several  coal  seams 
penetrated  are  no  less  than  14  or  15  in  number,  and  fall  into  three 
groups.  The  lower  groups,  consisting  of  five  coals  probably  of  small 
size,  includes  the  coals  from  670  to  850  feet  below  the  surface.  It  prob- 
ably includes  coals  1  and  2  of  northern  Illinois.  The  middle  group  com- 
prises the  coals  from  430  to  580  feet  below  the  surface  and  no  doubt  in- 
cludes Coal  No.  6.  The  uppermost  group  of  coal  beds,  comprising  some 
small  coals  of  the  "Upper  Coal  Measures"  of  Worthen,  are  the  coals  in 
the  upper  200  feet  of  the  section.  The  sandy  shale  in  the  lower  part  of 
the  section,  which  contains  the  oil  sand,  exhibit  a  quite  persistent 
lamination  of  thin  dark  and  light  layers.  It  is  believed  that  this 
feature  may  be  useful  in  their  identification  in  the  nearest  outcrops." 

No.  3.— L.  R.  Newlin,  No.  21. 
Location— SW.  %  SE.  %  sec.  27,  T.  6  N.,  R.  14  W.,  Martin  Township. 
Elevation— 498  feet. 

Depth  in  feet. 
From  To 

Drift     1  25 

Dark   limestone,    brown   limestone,    fragments    of   coal   and   yellow  • 

sand    25  30 


blatchleyJ  CRAWFORD   COUNTY   LOGS. 

Logs — Continued. 


Dark  limestone  with   sand    / 

Gray    sandstone   with   infiltrated   lime    

Gray  sandstone,  some  yellow  limestone,  and  siderite 

Gray  sandstone  with  some  yellow  limestone.     Pyrite  noted 

Coarse  gray  micaceous  sand  with  fragments  of  coal 

Coarse   gray  micaceous   sand    

Coarse   micaceous   sandstone    

Coal  and  some  fire  clay    

Gray  micaceous  sand.     A  little  lime  in  sand 

Dark   micaceous    shale   and   sand    

Gray  micaceous  shale  and  sand.     A  few  fossil  fragments 

Limestone,    fragmental,    organic,    crinoid    fragments    and    bryozoa 

noted     

Light  gray  shale  of  fine  texture    

Limestone,  in  part  fragmental,  and  some  shale    

Gray  sandy  shale  with  some  crinoidal  limestone   

Gray  micaceous  sandy  shale,  with  some  limestone    

Gray   micaceous   shale    

Gray  micaceous  sandstone  and  much  darker  clay  iron  stone 

Gray  micaceous  shaly  sandstone,  with  imbedded  shreds  of  vege- 
tation      

Gray  micaceous   shaly  sandstone    

Fine  grained,  gray  micaceous  sandstone  with  intersticial  lime.  .  .  . 
Some  black  fissile  shale.     Mostly  a  dark  blotched  organic  breccia 

limestone,   containing  many  crinoid   stems,    some  small  Athyris 

and  some  crinoid  spines    

Like  the  preceding,  with  some  sandstone  and  coal    

Sandstone,   limestone   and   shale    

Micaceous  sandstone,  with  some  laminated  sandy  shale 

Gray  sandstone,  quite  coarse   

Micaceous   silty   gray   shale    

Gray  shale,  and  some  dark  shale    

Black  shale,   clay  iron  stone,   crinoid   stems,   Bellerophon,   Athyris, 

a    cyathophylid,    two    gastropods     

Black  shale  and  coal    

Yellowish    and    gray    concretionary    siderite    and    limestone,    with 

some  fire   clay  and  coal    

Gray    shale    

Gray  sandstone  and  some  dark  shale    

Gray    micaceous    sandstone    

Laminated  gray  sandstone  of  fine  texture    

Gray  shale  and  fire  clay 

Gray   sandstone    

White   sandstone   with   siderite   concretions    

Laminated    sandstone 

Micaceous  sandstone   and  dark   shale 

White   micaceous   sandstone    

Gray  sandy  shale,   micaceous    

Gray  micaceous  sandy  shale  and  some  dark  gray  shale 

Like  the  preceding  with  some  clay  iron  stone    

Mostly    coal,    some    shale    and    some    fragments    of    concretionary 

limestone    

Gray   sandstone   with    siderite    

Gray  sandy   shale,   micaceous    

Gray   sandstone,    with    some   limestone,    white    

Gray    sandstone,    with    interstical    calcareous    material    and    some 

pure    white    limestone 

Greenish    gray    sandstone    

Gray    sandstone,    with    many    concretionary    spherules    about     % 

millimeter   in    diameter    

Gray   sandstone    

Dark  gray  sandy  shale,  stiff   

Dark  gray  micaceous   shale    

Dark    gray    shale 

Dark  shale  and  limestone,   with   pyrite   calcite  with  many  crinoid 

stems,  and  an  Estheria    (?)    , 

Coal  with  some  limestone   fragments  and  shale    

Coal   and   fire   clay    

Gray    sandstone,    with    some    yellow    fragments    or    concretionary 

material    " 

Gray     sandstone 

White    sandstone 

Yellowish  white   sandstone 

Dark    shale 

Black   shale   and   coal 

Gray   sandstone,   micaceous    

Gray  limestone  and  some  large  quartz  grains 

Gray   sandy   shale,    micaceous 


39 


Depth  in 

feet. 

From 

To 

30 

40 

40 

45 

45 

50 

50 

60 

60 

65 

65 

70 

70 

75 

75 

80 

80 

110 

110 

115 

115 

120 

120 

125 

125 

130 

130 

135 

135 

140 

140 

145 

145 

150 

150 

155 

155 

160 

160 

170 

170 

175 

175 

180 

180 

185 

185 

190 

190 

195 

195 

210 

210 

240 

240 

245 

245 

250 

250 

255 

255 

260 

260 

265 

265 

270 

270 

275 

275 

280 

280 

285 

285 

290 

290 

295 

295 

300 

300 

305 

305 

330 

330 

345 

345 

350 

350 

355 

355 

360 

360 

365 

365 

375 

375 

380 

380 

385 

385 

390 

390 

395 

395 

400 

400 

405 

405 

410 

410 

415 

415 

420 

420 

425 

425 

430 

430 

435 

435 

440 

440 

445 

445 

450 

450 

455 

455 

460 

460 

465 

465 

470 

470 

475 

40 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE   COUNTIES,   [bull.  no.  22 


Logs — Continued. 


Depth  in  feet. 
From  To 

Sandstone    and   some    limestone ( 475  48O 

Shaly  sandstone,  with  some  siderite  concretions . .' 480  485 

Black    and    dark    micaceous    shale 485  490 

Black    dolomitic    limestone,    with    calcite,    Rhombopora,    lepideden- 

droides,    crinoid    stems 490  495 

Black   limestone,   with   crinoid   stems   and   coal 495  500 

Gray   micaceous   sandstone,   with   some   interstical   calcareous   ma- 
terial   500  510 

Gray   sandstone   and   a    dirty   yellow   dolomitic   limestone,    concre- 
tionary   (?) 510  515 

Limestone     515  520 

Gray  silty  shale  with  carbonaceous  shreds  imbedded 520  525 

Gray   silty   shale   with   thin   layers   of   shiny    coal   of   silky   lustre. 

Coal  layer  in  one  fragment  adhering  to  the  shale 525  530 

Gray  shale   of  fine  texture 530  535 

Bark  shale  of  fine  texture 535  555 

Black   shale  and  coal,   mostly   impure 555  560 

White  sandstone  of  fine  texture 560  565 

Light  gray  shale,   with  small  spherical  siderite  concretions 565  570 

Gray  shale,  with  much  siderite,  in  fragments  and  in  minute  spher- 
ical concretions.     Some  bright  red  fragments  noted,   "rusty" 570  575 

Shaly  sandstone   and  sandy  shale,   gray,   with   siderite   as   in   pre- 
ceding   sample 575  58O 

Sandy  shale,  gray,  with  siderite  fragments 580  585 

Gray   sandstone,   some   shale   and  siderite 585  590 

Shaley  sandstone  or  sandy  shale,  gray 590  595 

Sandstone,    black   shale   and   "clod,"   with   some   coal   and   siderite 

concretions    595  605 

Shale  and  shaly  sandstone,  with  fragments  of  siderite  concretions 

and     coal 605  610 

Greenish  fire  clay  and  shale 610  615 

Shaly    sandstone,    gray 615  620 

Black  miner's  slate,   with  siderite  concretions 620  625 

Black  miner's  slate,  with  sandstone  and  gray  shale 625  630 

Gray  sandy  shale 630  635 

Dark  gray  sandy  shale,  micaceous 635  645 

Gray    laminated    shaly    sandstone 645  650 

Dark  gray   sandy   shale 650  655 

Black   stiff   shale,    almost   miner's    slate 655  665 

Black  stiff   shale   and  impure   coal 665  670 

Black  shale  and  black  concretionary  limestone,  with  fossils 670  675 

Gray  sand  and  gray  sandy  shale  with  some  coal 675  680 

Coal  with  very  bright  (black)   lustre  and  fire  clay 680  685 

Coal   of   bright  lustre   and  brownish  earthy  streak   and   some   fire 

clay    685  690 

Gray  gritty  fire  clay  and  dark  shale 690  695 

Shale,     gray 695  705 

Shale,  gray,  and  some  siderite 705  710 

Dark   limestone,    some   dark   shale   and   pyrite 710  720 

Dark   shale,   some   dark   limestone  and   spherulitic   siderite 720  725 

Shale,  dark,  some  coal;  a  little  dark  limestone 725  730 

Dark  shale,   some  coal,   and   spherulitic  siderite 730  735 

Gray  micaceous  shale,   and  bits   of  yellow  limestone 735  740 

Gray  micaceous  shale,   and  fragments  of  siderite 740  745 

Dark  micaceous  shale,  some  siderite,  bits  of  coal  and  lime 745  750 

Gray   micaceous   shale   and   siderite 750  755 

Gray  micaceous  shale,   some  fire  clay,   coal  and  pyrite 755  760 

Coarse  gray  micaceous   shale,   pyrite,   little   shale 760  770 

Black   shale  and  some  coarse   sandstone 770  775 

Coal  and  fire  clay,  and  some  gray  shale 775  780 

Coal  and  fire  clay,  and  some  gray  fire  clay  with  pyrite. 780  785 

Black  shale,   bits  of  yellow  limestone,   and  spines  of  brachiopods, 

and   spherulitic   siderite 785  790 

White  sandstone  and  shale,  black,  some  yellow  limestone  and  coal, 

and   spherulitic   siderite 790  795 

Dark  shale,   some  little  sandstone,   siderite  and  limestone 795  800 

Black  shale  and  some   siderite 800  810 

Black   shale 810  820 

Gray  micaceous  shale  and  some- sandstone 820  825 

Limestone,   dark  and  white  ;   some  sandstone  with  infiltered  lime ; 

gray  micaceous  shale,  pyrite  and  some  crinoid  joints 825  830 

Dark    and    white    limestone    with    crinoid    stems    and    pieces    of 

shells,    and    pyrite 830  835 

Gray  micaceous  sandstone,  and  some  dark  and  white  limestone...  835  840 

Black  micaceous  shale,  some  sandstone,  and  white  limestone 840  845 

Black    micaceous    shale 845  850 

Black  micaceous  shale,   some  white   sand  and  siderite 850  860 

Gray  sandstone  and  dark  shale 860  865 

Gray  sandstone,   some  dark  shale  and  siderite 865  870 


blatchley]  CRAWFORD    COUNTY   LOGS. 

Logs — Continued. 


Coarse  gray  sandstone  and  a  little  shale 

Gray  micaceous   sand 

Gray  sand  and  some  dark  shale 

Gray  sand,  white  limestone,  a  little  shale  and  pyrite. 
Gray  sandstone,  bits  of  limestone,   shale  and  siderite, 

Gray   micaceous   sand 

Gray  micaceous  sand,  and  some  dark  shale 

Dark  sandy  micaceous  shale 


41 


Depth  in 

feet. 

From 

To 

870 

875 

875 

885 

885 

890 

890 

895 

895 

905 

905 

940 

940 

950 

950 

955 

No.  4. — C.  E.  Siler,  No.  4. 

Location — NE.  corner  sec.  5,  Honey  Creek  Township. 
Elevation — 495  feet  (estimated). 

Pleistocene: 

Loess   or   yellow   loam 

Gravel   and   sand 

Sand  and  gravel 

Sand  and  gravel  washed  from  boulder  clay 

Boulder    clay 

t:Coal  Measures' : 

Limestone,  with  imbedded  crinoid  stem,  a  small  Spirifer  cam- 
eratus,  a  small  gasteropod,  and  a  piece  of  a  plant  stem. 
Some    roof    shale 

Shale,   greenish  gray,   micaceous 

Gray    shale 

Fine-grained  micaceous  sandstone  with  a  calcerous  matrix... 

Arenaceous,    gray    shale 

Micaceous,    gray   shale 

Micaceous,  dark  gray  shale 

Micaceous  sandstone,  with  fragments  of  concretions  of  car- 
bonate   of    iron 

Sandstone,  gray  micaceous,  calcareous  and  shaly,  with,  many 
fragments  of  shells  of  yellowish  color 

Gray  shale  and  micaceous  shaly  sandstone,  with  a  small  Mya- 
lina,  and  many  fragments  of  shells.     Some  coal  noted 

Some  limestone,  but  mostly  shale.  The  shale  is  dark  gray, 
micaceous,  and  marly.  It  has  many  minute,  apparently 
concretionary  grains,  yellow,  of  carbonate  of  iron.  These 
appear  like  coarser  grains  in  a  fine  textured  matrix.  The 
limestone  is  dark  with  imbedded  flat  fragments  of  Myalina, 
shells,  and  one  piece  was  seen  with  imbedded  trenchantly 
marked  tubules,  believed  to  be  irregularly  curving  forms  of 
Ammodiscus,  measuring  from  .1  to  .15  mm.  in  diameter.... 

Micaceous  sandstone  or  sandy  shale,  with  some  brownish 
limestone    

Micaceous  gray  sandstone  of  fine  texture,  almost  a  shale 

Micaceous  sandstone  and  some  green  grains,  with  some 
brown   calcareous   coaly   fragments 

Fine-grained  sand,  micaceous,  and  with  brown  and  green 
grains,    as    above 

Like  the  previous,  but  with  occasional  carbonaceous  frag- 
ments     

Gray,  micaceous  sandstone,  with  some  dark  and  some  green 
grains,   and  some  shreds  of  carbonaceous  material 

Black  fissil  "miner's  slate"  with  pryitized  fossil  shells,  one 
probably  being  an  Aviculopeaten,  another  like  a  minute 
Myalina    

Some  shaly  fire  clay  and  a  little  coal,  but  chiefly  gray  mica- 
ceous shale  with  minute  concretions  of  carbonate  of  iron 
of  the   size  of  small   sand  grains 

Gray  micaceous  shaly  sand.  One  large  fragment  showing 
lines  believed  to  be  wave  marks 

Gray  slightly  micaceous  shale,  with  very  thin  calcareous 
laminae     

Gray  shale,  slightly  micaceous  shale  with  a  brownish  minute 
disc-shaped  fossil  of  spiral  structure,  probably  an  Ammo- 
discus    

Gray  shale,  faintly  micaceous 

Black  fissile  shale,  with  a  very  fine  rectangular  reticulation 
seen  on  a  cleavage  plane.     Soma  fragments  of  coal 

Greenish  gray  fire  clay  and  shale,  with  fragments  of  dark 
concretionary   limestone 

Fine-grained  micaceous  sandstone  or  shale,  with  yellow 
specks   of  concretionary  siderite 


Depth  in 

feet. 

From 

To 

1 

5 

5 

10 

10 

15 

15 

20 

20 

40 

40 

45 

45 

50 

50 

55 

55 

62 

62 

68 

68 

74 

74 

80 

SO 
86 


'J  2 


150 


86 


98 


103 


103 
109 

109 
114 

114 

119 

119 

139 

139 

145 

145 

150 

155 


155 

160 

160 

165 

165 

170 

170 
175 

175 
180 

180 

185 

185 

190 

190 

200 

42 


OIL  FIELDS  OF  CRAWFOUD  AND  LAWRENCE   COUNTIES,    [bull.  no.  22 


Logs — Continued. 


Coal  Measures — Continued. 

Gray,  dark,  and  compact  concretionary  carbonate  of  iron  in 
large    fragments 

Dark  gray  shale,   with  Ammodiscus    (?)    

Mostly  dark  concretionary  carbonate  of  iron  in  large  frag- 
ments, with  some  dark  stony  shale    

Dark   shale    of  fine    texture    

Dark  shale  slightly  micaceous,  with  Ammodiscus  ( ?)  and 
minute  shreds  of  other  fossils   

Dark  micaceous   shale,   slightly   calcareous    

Like  the  previous,  with  minute  shreds  of  vegetation 

Dark  micaceous  shale,  like  that  in  the  previous  sample,  with 
Ammodiscus   (  ?)   and  a  small  ostracod 

Dark  micaceous  shale,  with  impressions  of  fern  leaves,  and 
with  a  spiral  Ammodiscus  (?)  and  one  tube  of  an  Ammo- 
discus (?)  only  slightly  curving.  Some  kealed  impressions 
were  noted  on  one  fragment  and  stem  joints  and  spines  of 
crinoids   were    also    noted    

Dark    gray    shale     

Gray  sandy  shale    

Gray  sandy  shale,  or  shaly  sandstone,  showing  some  dark 
grains   under   the   lens    

Shale,   greenish  gray,   sandy  and  micaceous    

Greenish  gray  micaceous  sandstone  and  red  clay  marl 

Greenish  gray  sandy  shale    

Comparatively  coarse  sandstone,  with  some  green  and  some 
pink  grains.  Also  some  lumps  of  fire  clay,  which  contain 
small  spherical  nodules  of  black  oxide  of  manganese  from 
one-fourth  to  one-third  mm.  in  diameter.  Some  of  these 
concretions  are  grown  together  in  groups  of  two  and  three 

Comparatively  coarse  sandstone,  with  some  interlaminated 
shale    

Mostly  sandstone,  gray  and  of  fine  texture,  with  some  shale. 
Color  various    

Sandy   gray   shale ,  or  shaly   sandstone    

Micaceous   gray    shale    

Dark  gray  shale,   not  micaceous    

Very  dark  shale,  carbonaceous  and  sandy.  Most  of  it  is 
finely  laminated  and  shows  shreds  of  vegetation   

Shaly  sandstone  or  shale,  thinly  laminated,  containing 
brownish  yellow  grains  (concretionary?)  larger  than  the 
grains  of  the  rock  and  also  some  still  larger  black  grains.  . 

Like  the  previous,  with  the  brown  grain  least  abundant  in 
the  layers  of  the  finest  texture,  which  are  carbonaceous.  .  . 

Sandstone,  with  interlaminated  carbonaceous  streaks  show- 
ing vegetable    tissue    .  .' 

Coal,    shale,    and   sandstone    

Mostly    fire    clay    

Mostly  concretionary  material,  carbonate  of  lime  and  iron, 
and   some    shale    

Concretionary  limestone  and  carbonate  of  iron,  in  shale 

Light  gray  micaceous  and  sandy  shale   

Micaceous   and  sandy  gray  shale    

Micaceous   sandstone   and   gray   shale    

Dark  gray  shale    

Dark  gray  limestone,  consisting  of  organic  fragments,  some 
black  shale  and  coal.  The  limestone  contains  Chonetes 
mesolobus  (?),  crinoid  stems  and  a  gasteropod  (Bellerophon 
carnonaria?)      

Fire  clay,  gray  and  black  shale,  and  coal    

Gray    shale    

Gray  sandstone  of  fine  texture    

Gray   shale,    arenaceous   and   micaceous    

Shaly  sandstone,  micaceous  and  with  rusty  specks   

Gray  shale,  micaceous   and  sandy    

Dark  gray  shale,  micaceous  and  sandy   

Like  the  above,  but  darker 

Almost  black  dolomitic  limestone,  uniform  in  texture,  emits 
sulphurous  odors  when  heated  and  becomes  slightly  magnetic 
before  the  blowpipe,  and  contains  joints  of  crinoid  stems, 
Chonetes  mesolobus  (?)  Rhombopora  lepidodendroides  (?). 
fragments  of  brachiopod  shells,  and  Fusulina  of  the  kind 
occurring  in  the  limestone  above  Coal  number  6 

Black  fissile  shale  and  some  coal,  with  limestone 

Gray  sandy  shale  and  some  dark  shale    

Gray  slightly   sandy   shale    

Soft    gray   micaceous    shale    

Gray  shale,  soft  and  micaceous,  with  some  dark  shale  show- 
ing shreds  of  vegetation    


Depth  in 
From 

feet. 
To 

200 
205 

205 
210 

210 
215 

215 

220 

220 

225 
230 

225 
230 
240 

240 


245 
250 
255 

260 
265 

270 
275 


280 
286 


120 


245 


25  0 
255 
260 

265 
270 
275 
280 


290 


290 

295 

295 

302 

302 

30S 

308 

320 

338 


338 

350 

350 

356 

356 

362 

362 

368 

368 

374 

374 

380 

380 

387 

387 

394 

394 

401 

401 

407 

407 

413 

413 

4L9 

419 

426 

426 

432 

432 

43S 

438 

450 

450 

456 

456 

462 

462 

468 

468 

480 

480 

486 

486 

492 

492 

498 

498 

504 

504 

510 

510 


516 


534 

540 

540 

546 

546 

552 

552 

564 

564 

570 

570 

576 

576 

588 

588 

594 

594 

600 

600 

606 

606 

612 

612 

618 

618 

624 

624 

636 

636 

642 

blatchlet]  CRAWFORD   COUNTY   LOGS.  43 

Logs — Continued. 

Depth  in  feet. 
From  To 

Coal  Measures — Continued. 

Gray  slightly  micaceous  sandstone,  with  some  large  and  thin 

fragments  of  black  dolomitic  limestone    516  522 

Gray  sandstone,  with  some  limestone  like  that  in  the  pre- 
vious   sample     522  528 

Dark  gray  highly  micaceous  shale,  with  scales  of  biotite  and 
on  fresh  fractures  having  an  appearance  like  that  of 
Archaen    schists    528  534 

Gray  sandstone  and  sandy  micaceous  shale,  with  some  dark 
shale  and  fragments  of  coal    

Dark  gray  sandy  shale,  micaceous,  with  some  fire  clay 

Dark  shale  of  fine  clayey  texture    

Dark  gray  shale,   micaceous  and  stony    

Dark   gray  shale,    of   clayey  texture    

Dark  gray  shale,  with  narrow  fucoid  bands  in  some  cleavage 
planes     

Black   fissile    shale    

Mostly  light  gray  sandstone,  some  gray  shale,  with  fragments 
of   coal   and  limestone    

Mostly  light  gray  sandstone  with  some  dark  shale 

Dark   micaceous,    shaly   sandstone    

Dark  micaceous,    sandy   shale    

Dark,  almost  black,  shale   

Dark,  almost  black,  shale,  with  fragments  from  concretion 
of  carbonate   of   iron    

Gray  shale,   of  clayey  texture    

Gray  shale,  with  some  little  mica    

Like   the    previous    sample,    but    slightly    coarser   and    with    a 

little   more   mica    642  648 

Black   shale,    of   fine   texture,    but   with   some   mica,    and  with 

earthly   lustre    648  654 

Black  shale,  much  pyrites  of  iron,  and  some  coal.  The  shale 
has  imbedded  calcareous  fossils  among  which  a  piece  of 
lamellibranch  valve  and  a  Bellerophon  were  noted,  and 
also  impressions  of  an  insect  wing  (?).  In  the  fragments 
of  pyrites  was  noted  a  Nucula,  a  Bellerophon  carbonaria 
(?)    in    part    filled    by    zinc    blende,    and    a    fragment    of    a 

brachiopod.     In  the  coal  some  woody  tissue  was  noted 664  660 

Light    gray    sandy    fire    clay    filled    with    small    crystals    of 
pyrites     

Dark   gray  micaceous  and  sandy   shale    

Dark  gray  shale  of  fine  texture,  with  pyrites  and  coal 

Black  fissile  shale  and  finely  laminated  coal  with  brown 
streak.     Woody  fibre  seen  in  some  pyrite    

Shaly  fire  clay,  light  gray  and  stony 

Gray   shale   and   sandstone    

Sandstone,  somewhat  coarse,  laminated,  in  alternate  layers 
of  white  and  carbonaceous  black  material,  some  layers 
micaceous     

Dark  gray  shale,  stony,  sandy  and  micaceous    

Gray  shale,  stony,   sandy  and  micaceous    

Dark  shale,  with  some  laminated  coal  and  some  fire  clay 

Gray  sandstone,   shaly  and  micaceous    

Soft   gray  shale    

Some  gray  shale,  and  some  dark  micaceous  shale  with  con- 
cretionary carbonate  of  iron   

Almost  black  fissile  shale,  with  concretionarv  carbonate  of 
iron    

Gray   sandstone   of  fine   texture    

Dark  gray  shale,   arenaceous  and  micaceous    

Laminated,  gray  sandstone,  micaceous,  alternate  layers  in 
black  and  carbonaceous,  the  black  layers  very  thin,  the 
light  layers  in  several  cases  measuring  one-tenth  of  an 
inch   in  thickness    762  768 

Coarse  micaceous  sandstone,  laminated  with  alternate  layers 
of   dark    carbonaceous   shale    

Like  the  previous,   sandstone  coarser  and  softer   

Dark  gray  shalo  and  some  lighter  shale    

Almost  black  shale,   fine  in  texture    

Light  gray  sandy  shale,   slightly  micaceous    

Dark  gray  and  light  gray  shale  of  fine  texture   

Gray  sandstone,  of  very  fine  texture   

Dark  bluish  gray  shale  of  very  fine  texture  with  concretionary 
carbonate   of   iron    

Almost  black  shale,  very  fine  in  texture   

Coarse   sandstone    

Almost  black  shale,  fine  in  texture    

Almost  black  shale,  with  biotite    

Black  shale,  fine  in  texture    

Gray   sandstone,    fine   grained    


660 
666 
672 

666 
672 

678 

678 
684 
690 

684 
690 
696 

696 

708 
714 
720 
726 
732 

70S 
714 
720 
726 
732 
738 

738 

744 

744 
750 
756 

750 
756 
762 

768 

786 

786 

798 

798 

804 

804 

817 

817 

830 

830 

836 

836 

848 

848 

854 

854 

860 

860 

866 

866 

878 

878 

884 

884 

902 

902 

908 

44  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 

Logs — Continued. 

Depth  in  feet. 
From  To 

Coal  Measures — Concluded. 

Gray  sandstone    908  914 

Black    shale    of    fine    texture,    with    concretions    of    carbonate 

of   iron 914  93S 

Gray    shale    and   sandstone,    with    some   large    and    thin    chips 

of  coal    938  944 

Gray  soft  sandstone  and  shale.  The  rock  in  this  and  the 
previous  sample  appears  to  be  a  mixture  of  alternating 
layers  of  shale  and  sandstone 944  950 

Gray  soft  sand,  only  a  single  fragment  of  loosely  coherent 
rock,  remaining  in  the  sample.  Size  of  grains  is  about 
one-fourth  mm.  in  diam.  Apparently  oil  sand ;  the  grains 
float  on  water    950  955 

Gray  sand,  with  grains  mostly  from  one-eighth  to  one-half 
mm.  in  diameter.  The  largest  grains  all  have  crystalline 
facets  resulting  from-  secondary  growth.  Sand  floats  on 
water    955  959 

Sand  like  the  previous,  but  faintly  brownish  yellow 959  963 

Sand  like   that   in  the   three   previous   samples,   except   that  it 

is  more  nearly  white  in  color    963  967 

Note; — Dr.  Udden  states  that  two  specimens  of  a  Fusulina  were 
found  in  a  limestone  occurring  at  the  depth  of  480  to  486  feet  from 
the  surface,  and  this  no  doubt  is  the  limestone  which  forms  the  cap- 
rock  over  Coal  No.  6.  The  rock  itself  has  been  altered  to  a  dark 
dolomite,  effervescing  very  tardily  in  acid.  It  has  a  dark  gray  color 
which  is  evidently  due  to  the  presence  of  iron  pyrites  in  microscopic 
particles.  On  heating  in  a  closed  tube  it  gives  off  sulphurous  odors  and 
becomes  slightly  magnetic.  The  entire  section  represented  by  the  two 
samples  studied  consists  of  variations  of  shales,  sandstones,  limestones, 
coals  and  fire  clays,  with  calcareous  concretionary  matter,  and  more  fre- 
quently concretions  of  carbonate  of  iron.  They  all  have  the  general 
appearance  characteristic  of  the  Pennsylvanian  series  in  this  region. 
About  a  dozen  coal  beds  were  penetrated,  which  occur  in  three  groups, 
not  counting  an  evidently  thin  bed  of  somewhat  shaly  coal,  which  lay 
at  a  depth  of  904  feet  below  the  surface  and  only  a  few  feet  above  the 
oil  sand.  The  lowest  of  these  groups  which  presumably  includes  equiva- 
lents of  Coals  Nos.  1  and  2  in  northern  Illinois,  is  represented  by  three 
seams  at  720,  678  and  660  feet  below  the  surface.  The  middle  group, 
which  includes  Coal  No.  6  is  represented  by  one  coal  at  540  feet,  by 
Coal  No.  6  at  the  depth  of  485  feet,  another  coal,  overlain  by  limestone, 
at  420  feet  and  a  coal  overlain  by  sandstone  at  365  feet.  The  coal  beds 
of  the  "Upper  Coal  Measures"  of  Worthen  are  represented  by  an  ap- 
parently small  seam  of  coal  at  a  depth  of  185  feet,  one  small  coal 
associated  with  a  capping  calcareous  bed  at  the  depth  of  95  feet,  and  a 
black  shale  under  a  limestone  at  the  very  surface  of  the  bed  rock  under 
the  drift,  fifty  feet  below  the  surface.  The  spiral  shell  of  an  Ammo- 
discus  was  observed  in  cleavage  surfaces  of  some  shales  in  the  "Upper 
Coal  Measures"  and  presumably  the  same  fossil,  in  the  form  of  irregu- 
larly bending  tubes  occurred  in  some  limestone  at  the  depth  of  100  feet. 

No.  5.— C.  F.  Curtis,  No.  8. 

Location — NE.  corner  sec.  11,  Oblong  Township. 
Elevation — 475  feet  (estimated). 

Depth  in  feet. 

From  To 

Yellow  boulder  clay 1  10 

Boulder  clay  and  drift  gravel    10  15 

Drift   gravel   and   sand    15  20 

Drift  gravel  and  sand,   with   some  boulder   clay    20  25 


blatchlet]  CRAWFORD   COUNTY   LOGS. 

Logs — Continued. 


Drift    sand   and    gravel    

Drift    

Drift  sand  and  gravel    

Drift  gravel  and  some  sand    

Drift  sand  and  gravel.     A  few  bits  of  coal    

Drift   sand   and    gravel    

Drift  sand  and  gravel,  with  some  shale    

Sandy  micaceous   shale    

Dark   micaceous    shale    

Sandy   dark    gray   shale    

Sandstone,    sandy   shale   and   coal.      Some   fragments   of  limestone 

noted  and  some  pyrites  with  woody  fibre    

Black  shale,  fire  clay  and  coal 

Gray  and  yellow  limestone.     Gray  sandstone  and  coal  with  some 

shale     

Gray  sandstone,  micaceous  and  of  fine  texture   

Like   the   preceding,   with  some   siderite    

Moderately  coarse   gray  and  yellow  micaceous   sand 

Gray  shale,  micaceous  sand   

Moderately    coarse   micaceous    sandstone    

Gray,  fine  sandstone,  and  yellow  concretionary  limestone,  in  which 

is   considerable    pyrite    

Gray  micaceous  sandy  shale  and  concretionary  siderite   

Gray  micaceous  sandy  shale  and  a  few  pieces  of  yellow  limestone 

Gray  micaceous  sandy  shale    

Gray  micaceous   shale    

Gray  micaceous  shale,  a  few  pieces  of  gray  sandstone,  some  white 

limestone   and   coal    

Gray  micaceous  shale,  with  imprint  of  vegetation,   some   fire   clay 

and   pieces   of  white   limestone    

Dark  gray  micaceous  shale    

Dark  gray  and  gray  micaceous  shale    

Dark  micaceous   shale    

Black  shale,  a  few  pieces  of  sandstone,   siderite,   yellow  limestone 

and  pyrite    

Black  shale  and  coal,  some  pure  calcite  and  white  limestone 

Black  shale  and  coal,  some  dark  limestone  and  gray  sandstone.  .  . 
Darkish   gray   limestone    (nodular    in   structure),    some    coal    gray 

sandstone  and  bits  of  pyrite    

Gray  shale,  concretionary  yellow  limestone,  some  white  limestone, 

some  gray  sandstone,  and  some  black  coaly  shale    

Yellowish   limestone,    some    gray   limestone,    gray   sandstone,    some 

concretionary  sandstone,  a  little  coal  and  pyrite   

Greenish  gray  stony  shale,  with  a  few  very  thin  laminae  of  coal.  . 

Gray  micaceous  stony   shale    

Dark   gray  stony  shale 

Dark  greenish  gray  shale  of  fine  texture 

Dark  shale  of  fine  texture    

Gray  sandstone,    brown    concretionary   siderite,    gray    shale,    black 

shale,  gray  limestone,  crinoid  stems  and  a  few  fragments  of  coal 
Gray  shale  and  grayish  brown  fossiliferous  limestone,  with  crinoid 

stems,  brachiopod  spines,  pieces  of  shells,  etc.  A  piece  of  con- 
cretionary siderite  showed  a  fissure  filled  with  clear  calcite.... 
Gray    shale,    concretionary    brown    siderite,    sandstone    and    coal. 

The  limestone  contains  organic  fragments.      The   coal  is  impure 

and  shows  very  thin  lamination    

Gray   sandstone   containing   shreds   of   carbonaceous   material    and 

pyrite,  with   some   shale    

Light    gray    thin-bedded    micaceous    sandstone,    some    pieces    with 

infiltrated    lime     ., 

Mostly  a  grayish  limestone  containing  some  fine  siliceous  mate- 
rial,   with    some    yellow    and    some    white    limestone    and    some 

black  shale    

Gray    limestone    and    some    gray    sandy    lime,    showing    occasional 

obscure   fragments   of  fossils    

Gray  limestone  and  white  limestone  of  waxy  lustre    

Greenish  gray  micaceous  and  sandy  shale  and  some  lime 

Greenish   gray  shale  of  somewhat  fine  texture    

Dark  gray  shale  of  somewhat  fine  texture    

Gray    shale    

Dark   almost  black  micaceous   shale,   showing   narrow   traversions 

impregnated  with  thin  green  films  of  pyrite    

Black   shale  with  shreds  of  carbonaceous  vegetation.      Some   gray 

shale   and   some   siderite    

Gray    shale    with    carbonaceous    shreds,    some    black    coaly    shale. 

A   few  pieces  of  siderite  noted    

Gray  and  black,  coaly  shale  and  gray  sandstone    

Gray  sandstone,  some  gray  shale  and  pieces  of  siderite   


45 


Depth  in 

feet. 

From 

To 

25 

30 

30 

35 

35 

60 

60 

70 

70 

75 

75 

90 

90 

110 

110 

115 

115 

120 

120 

135 

135 

140 

140 

145 

145 

150 

150 

155 

155 

165 

165 

170 

170 

180 

180 

190 

190 

195 

195 

205 

205 

210 

210 

215 

215 

220 

220 

225 

225 

230 

230 

235 

235 

240 

240 

245 

245 

250 

250 

255 

255 

260 

260 
265 


310 

315 

320 
325 
335 

345 


265 
270 


270 

275 

275 

280 

280 

290 

290 

295 

295 

305 

305 

310 

315 

320 

325 
335 
345 

350 


350 

355 

355 

360 

360 

380 

380 

385 

385 

395 

395 

400 

400 

405 

405 

410 

410 

415 

415 

425 

425 

435 

435 
440 
445 
455 

440 
445 
455 
460 

460 

465 

465 

475 

475 

480 

480 
485 

485 
490 

495 

490 

495 
500 

500 

505 

505 

510 

515 

520 

520 

525 

525 
530 

530 

550 

46  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE   COUNTIES,   [bull.  no.  22 

Logs — Continued. 

Depth  in  feet. 
From  To 

Gray  micaceous  sandy  shale,  some  gray  shale  and  concretionary 
siderite    

Dark  gray  shale 

Dark  gray  shale  and  concretionary  siderite    

Dark  gray  shale,  with  imprints  of  vegetation,  and  some  siderite .  .  . 

Gray  shale  with  imprints  of  vegetation.  Some  siderite  and 
some    carbonaceous    shale    

Gray  sandstone  and  white  limestone,  some  fragments  of  coal  and 
of  concretionary  siderite 

Gray  micaceous  shale,  some  yellow  concretionary  siderite,  a  little 
limestone  and  gray  shale 

Gray  micaceous  sandy  shale,  some  yellow  limestone  and  siderite.. 

Dark  gray  sandy  micaceous  shale,  some  gray  shale,  concretionary 
siderite  and  some  gray  sandstone 

Dark   micaceous    shale 

Dark  gray  micaceous  shale  and  some  siderite 

Black  limestone  and  some  black  shale,  and  some  siderite.  Crinoid 
stems   noted 

Black  limestone,  some  black  shale,  some  coal  and  siderite.  Crinoid 
stems   noted 

Black  limestone,  some  black  shale,  coal  and  siderite.  A  Fusulina 
lamellibranch  ( ?)  shell,  Aviculopecten  carboniferous,  a  minute 
gasteropod,  and  some  crinoid  spines  and  stems  noted.  The  lime- 
stone yields  bituminous  and  sulphurous  odors  when  heated 510  515 

Dark  limestone,  some  pieces  impregnated  with  small  particles  of 
pyrite,  some  coal  and  black  shale,  some  siderite  and  fragments 
of  white   limestone   and   calcite 

Black  limestone,  a  few  pieces  of  coal,  pyrite,  siderite,  white  lime- 
stone and  crinoid  stems 

Gray  micaceous  sandstone,  some  black  limestone,  coal  and  gray 
shale  with  pyrite  siderite  and  white  limestone 

Gray  micaceous  sandstone 

White    micaceous    sandstone    with    some    concretionary    limestone 

and  bits  of  coal 550  555 

White  micaceous  sandstone  and  coal,  with  some  fire  clay,  siderite, 
white  limestone,  much  pyrite,  and  some  calcite.  Productus, 
Edmondia  nebrascensis  (?),  Hemipronitus  crassus,  Chonetes 
punctatus  (?),  some  small  gasteropods,  several  crinoid  spines 
and  stems  and  a  bryozoan  like  Rhombopora  noted 555  560 

Gray    sandstone    and    coal,    with    some    white    limestone,    pyrites, 

calcite,  shale  and  a  few  crinoid  stems 560  565 

Dark  gray  shale,  some  coal,  sandstone,  pyrite  and  fire  clay 565  570 

Gray  micaceous  sandstone,  with  a  little  fire  clay  and  shale 570  575 

Gray  micaceous  sandstone,  some  of  which  is  studded  with  spher- 
ules of  pyrite  measuring  from  1  to  3  mm.  in  diameter,  and 
showing  faces  of  small  cubic  crystals  on  the  surface 575  585 

Gray    micaceous    shale 585  610 

Gray  micaceous  shale  and  some  siderite 610  615 

Dark  gray  shale 615  620 

Gray  shale  and  some  yellow  limestone,  concretionary  siderite  in 
large  fragments  and  in  minute  spherules,  coal  and  some  sand- 
stone      620  625 

Gray   micaceous   shale,    a   little   yellow   limestone,    siderite,    pyrite 

and   coal 625  630 

Gray  micaceous  sandstone  and  shale  with  siderite,  fire  clay  and 
coal    

Gray  micaceous  sandstone  and  some  shale 

Gray  micaceous   sandstone 

Gray  micaceous  sandstone,  with  some  siderite 

Gray  micaceous  shale  and  some  yellow  limestone,  and  fire  clay. . .  . 

Dark  gray  shale,  some  fire  clay  and  concretionary  siderite 

Dark  gray  micaceous  shale  and  a  little  yellow  limestone  and 
siderite    

Dark  gray  micaceous  shale 

Dark  gray  and  some  micaceous  black  shale,  with  a  little  siderite.. 

Dark  shale,  with  imprints  of  vegetation,  and  some  fire  clay 

Dark  shale  and  concretionary  siderite 

Dark  micaceous  shale  and  some  siderite 

Dark  gray  micaceous  shale 

Gray  micaceous  shale  and  some  sandstone 

Gray  laminated  sandstone  and  black  shale 

Dark  shale,  concretionary  siderite  and  a  little  sandstone 

Hard  black   shale 

Black  shale,  some  coal  and  sandstone  and  a  little  siderite 

Gray  micaceous  shale,  some  yellow  limestone,  some  black  shale 
and  a  few  bits  of  coal 

Black  shale  and  a  few  fragments  of  yellow  limestone  and  coal 

Black   micaceous   shale 

Coal  and  a  few  pieces  of  black  shale 


630 

635 

635 

640 

640 

645 

645 

650 

650 

655 

655 

660 

660 

675 

675 

680 

680 

685 

685 

690 

690 

695 

695 

700 

700 

715 

715 

725 

725 

730 

730 

735 

735 

740 

740 

745 

745 

750 

750 

755 

755 

760 

760 

765 

blatchley]  CRAWFORD   COUNTY   LOGS. 

Logs — Continued. 


Coal    and   black    shale,    some    white    limestone,    a    little    sandstone 

siderite  and  bits  of  pyrite 

Gray  sandstone,  some  dark  shale,  bits  of  coal  and  limestone 

Gray  micaceous  sandstone  and  a  little  yellow  limestone 

Dark  micaceous  shale  and  a  little  siderite 

Black  shale  and. a  little  coal.     A  little  gray  limestone  noted 

Black  shale,  a  little  coal  and  a  little  sandstone 

Dark  pyritiferous  shale  and  some  gray  sandstone 

Gray  micaceous   shale 

Gray  micaceous  shale  and  a  few  bits  of  coal 


47 


Depth  in 

feet. 

From 

To 

765 

770 

770 

775 

775 

790 

790 

795 

795 

800 

800 

805 

805 

815 

815 

820 

820 

825 

No.  6.— J".  M.  Drake,  No.  23. 

Location — NE.  %  sec.  9,  Oblong  Township. 
Elevation — 490  feet    (estimated). 

Depth  in  feet. 

From  To 

Gray  limestone,  some  yellow  limestone  and  bits  of  shale 200  205 

White    and    yellow    limestone,    concretionary    siderite,    some    gray 

sandstone  and  a  piece   of   quartz 205  210 

Yellow  and  white  limestone,  gray  sandstone,  concretionary  siderite 

and  some   dark   shale 210  215 

Gray  sandstone,  some  yellow  sandstone,  siderite,  quartz  fragments, 

yellow  limestone  and  a  few  pieces  of  bright  green  sandstone....  215  220 
Yellow    limestone,    some    siderite,    shale    and    sandstone    and    red 

quartz    (from    drift?) 220  225 

White  and  yellow  limestone  and  a  few  pieces  of  dark  shale 225  230 

White  limestone 230  250 

Very  fine  micaceous  white  sand  and  limestone 250  270 

Dark  gray  micaceous  sandy  shale 270  275 

Dark  micaceous  shale 275  285 

Black  shale  and  gray  sandstone,  with  a  little  limestone 285  290 

Dark  limestone,  some  yellow  limestone  and  bits  of  coal 290  295 

Black  shale,  a  little  yellow  limestone  and  a  few  fragments  of  coal  295  300 

Gray  shale,  some  yellow  limestone  and  coal 300  305 

Gray  shale  and  some  yellow  limestone 305  310 

Gray    shale 310  315 

Gray  shale  and  some  yellow  limestone 315  320 

Gray    shale 320  330 

Gray  shale  and  a  little  yellow  limestone 330  335 

Gray  micaceous  shale  and  some  micaceous  sandy  shale 335  340 

Gray   shale 340  350 

Concretionary  siderite  with  a  little  yellow  limestone  and  shale.     A 

Cyathophylid  coral  noted 350  355 

Gray  shale  and  a  little  yellow  limestone 355  360 

Gray    shale,    yellow    limestone    and    some    sandstone.      The    shale 

contains  shreds  of  vegetation 360  365 

Gray  shale  and  concretionary  siderite 365  370 

Gray  limestone  and  some  gray  shale 3  70  375 

White  limestone.     A  crinoid  stem  noted 375  380 

White  limestone,  some  greenish  sandstone  and  a  few  bits  of  coal.  .  380  385 

Gray  micaceous  sandstone  and  white  limestone 385  390 

Gray  shale  and  a  little  limestone 390  395 

White   limestone  and  some  gray  shale 395  400 

Gray  shale  and  some  limestone 400  405 

Concretionary  siderite.  some  dark  shale,  bits  of  coal  and  pyrite....  405  410 

Gray  sandy  shale  and  siderite.     Some  yellow  limestone 410  415 

Dark  gray  shale,  some  siderite  and  yellow  limestone 415  420 

Gray  sandy  shale  and  some  siderite 420  425 

Gray  sandy  shale,  black  shale  and  some  siderite 425  435 

Gray  micaceous  sandstone  and  a  few  bits  of  yellow  limestone 435  440 

Gray  micaceous   sandstone 440  445 

Gray  micaceous  sandstone  with  shreds  of  vegetation.     A  few  small 

pieces   of   siderite 445  460 

Gray  micaceous  sandstone  and  a  few  small  pieces  of  white  lime- 
stone       460  465 

Gray  micaceous  sandstone  with  shreds  of  vegetation 465  470 

Gray  micaceous   sandstone,   some   dark   shale,   a  few  bits  of  coal, 

and   nyrite   showing  woody  tissue 470  475 

Gray    micaceous    sandstone    and   white    limestone.      A    little    dark 

shale   noted 475  480 

Gray  sandy  shale  and  yellow  limestone 480  485 

Gray  sandy  shale  and  white  limestone.  Some  yellow  limestone....  485  490 
Sandstone  with  infiltrated  lime,  white  limestone,   and  a  few  small 

spherical    siderite   concretions 490  495 


48 


OIL   FIELDS   OF   CRAWFORD  AND  LAWRENCE   COUNTIES,    [bull.  no.  22 


Logs — Continued. 


Gray  micaceous  sandy  shale,  some  yellowish  limestone,  white  sand- 
stone and  a  little,  dark  shale 

White  sandstone,  some  dark  shale  and  yellow  limestone 

Dark  gray   shale 

Dark  shale,  fire  clay,  and  some  white  limestone 

Dark    gray    shale 

Dark  limestone,  some  dark  shale,  crinoid  stems  and  some  other 
organic  material  noted.  Tuberculated- crinoid  spine  noted  like 
that  in  S.  G.  McCleave  well,  505-510,  Fusulina  noted 

Dark  limestone,  coal,  some  yellow  limestone  and  several  crinoid 
stems    noted 

Gray  micaceous  sandstone  and  a  few  pieces  of  coal 

Gray  micaceous  sandstone,  a  few  bits  of  coal  and  siderite 

Gray   micaceous   shaly  sandstone,  some  siderite  and  a  little  limestone 

Gray  shale 

Dark    gray    shale 

Gray  shale,  some  siderite  and  bits  of  pyrite 

Gray  shale  and  a  little  coal 

Black  shale  and  gray  micaceous  shale 

Black  micaceous  shale  and  gray  sandstone 

Gray  micaceous  sandy  and  some  black  shale 

Gray  micaceous  shale  and  black  shale 

Gray  micaceous  sandy  shale  and  a  little  black  shale 

Gray  micaceous  sandstone  and  some  siderite 

Gray  micaceous  shale,  some  sandstone  and  siderite 

Dark  micaceous  shale 

Gray  micaceous  shale  with  shreds  of  vegetation 

Gray  sandy  shale *».... 

Gray   shale 

Dark  gray  shale  and  some  siderite 

Dark  gray  shale,  some  siderite  and  yellow  limestone 

Dark  shale,  and  siderite  concretions 

Dark  shale,  some  siderite  and  a  little  white  limestone 

Gray   shale 

Gray  sandstone,  a  few  bits  of  pyrite  and  siderite 

Gray  sandstone 

Gray  sandy  shale 

Dark  shale  and  gray  sandy  shale 

Dark  gray  shale  and  some  siderite 

Dark   gray   shale 

Dark  shale  and  some  siderite 

Dark  shale,  and  a  little  siderite 

Dark  shale,   a  little  white  sandstone  and  siderite 

Dark  shale  and  concretionary  siderite 

Dark  shale 

Black  shale 

Black  shale  and  some  sandstone 

Gray  micaceous  sandstone  and  a  little  black  shale 

Gray  shale  and  micaceous   sandstone 

Gray  micaceous  shale  and  little  sand 

Coal  and  gray  shale 

Gray  shale,  some  fire  clay,  a  little  coal  and  bits  of  pyrite 

Gray  shale  and  some  gray  micaceous  sandstone 

jray  micaceous  sandy  shale  and  some  gray  shale 

Gray  micaceous  shale 

Gray  sandy  micaceous  shale 

Gray  shale  and  concretionary  siderite 

Coal     

Black  carbonaceous  shale  and  some  gray  shale 

Black  shale,  gray  sandstone  and  a  little  coal 

White  sandstone  and  a  little  white  limestone 

Dark  shale  and  some  white  sandstone  with  infiltrated  lime 

Dark  shale  and  some  white  sandstone  with  infiltrated  lime 

Dark    shale,    white    sandstone,    with    infiltrated    lime,    some    small 

Dark  shale,  white  micaceous  sandstone,  and  bits  of  coal 

White   micaceous   sandstone - 

Dark   shale  and  micaceous  sandstone 

Black  micaceous  shale,  a  little  white  limestone  and  a  few  bits 
tions    

Gray  micaceous  shale 

Hard  black  shale  and  a  few  pieces  of  white  limestone 

Gray  sandstone  and  black  shale.  Small  spherical  siderite  concre- 
tions  and  bits   of  pyrite 

Black  shale 

Black  shale  and  a  very  few  pieces  of  white  limestone 

Black  micaceous  shale,  white  sandstone  and  some  siderite  concre- 
of    coal 

Black  micaceous  shale  and  a  little  limestone 

White  sandstone  and  dark  shale 


Depth  in  feet. 

From  To 

495  505 

505  515 

515  520 

520  525 

525  530 


530 


540 


540 

545 

545 

550 

550 

555 

555 

560 

560 

565 

565 

570 

570 

575 

575 

580 

580 

585 

585 

590 

590 

595 

595 

600 

600 

605 

605 

610 

610 

615 

615 

620 

620 

625 

625 

635 

635 

640 

640 

645 

645 

650 

650 

655 

655 

660 

660 

670 

670 

680 

680 

685 

685 

690 

690 

695 

695 

710 

710 

715 

715 

725 

725 

735 

735 

745 

745 

755 

755 

760 

760 

765 

765 

770 

770 

775 

775 

780 

780 

785 

785 

790 

790 

795 

795 

800 

800 

810 

810 

820 

820 

825 

825 

830 

830 

835 

835 

840 

840 

845 

845 

850 

850 

860 

850 

860 

865 

870 

870 

875 

875 

880 

880 

885 

885 

890 

890 

895 

895 

900 

900 

905 

905 

91C 

910 

915 

915 

920 

920 

930 

BLATCHLET] 


CRAWFORD    COUNTY    LOGS. 


49 


Logs — Continued. 


White  micaceous  sandstone  containing  carbonaceous  shreds  and  a 
little   black   shale 

Dark  shale  and  some  white  micaceous  sandstone 

Like  the  preceding  with  a  few  bits  of  coal 

Dark  micaceous  shale 

White  micaceous  sandstone,  some  shale  and  a  few  bits  of  lime- 
stone     - 

Gray  micaceous  shale,  black  shale  and  some  sandstone 

Gray  shale  and  some  sandstone 

White  micaceous  sandstone  and  some  dark  shale 

Gray  micaceous  sandy  shale  and  a  few  pieces  of  white  limestone . . 

Gray  shale  and  some  sandstone .- 

Gray  shale 

Black  shale  and  a  little  gray  sandstone  with  infiltrated  lime 

Gray  micaceous  shale,  some  grayish  green  pieces  of  shale  and  a 
few  bits  of  limestone 

Dark  shale  and  a  little  sandstone 

Dark    shale ' 

Yellow  micaceous  sand 

Yellow  micaceous  sand  and  some  dark  shale 


Depth 

in  feet. 

From 

To 

930 

935 

935 

955 

955 

960 

960 

965 

965 

975 

975 

980 

980 

985 

985 

995 

995 

1,005 

1,005 

1.01Q 

1,010 

1,020 

1,020 

1,030 

1,030 

1,045 

1,045 

1,050 

1,050 

1,055 

1,055 

1,060 

1,060 

1,065 

No.  7— J.  E.  Wilson,  No.  21. 


Location— W.  %  NW.  %  sec.  17,  T.  7  N. 
Elevation — 490  feet  (estimated). 


R.  12  W.,  Robinson  Township. 


Depth  in 
From 

Dark   gray   shale,   fine    200 

Gray  shale,   fragments  of  concretions  and  coal    205 

Shale,   sandy,   micaceous,   light   gray    210 

Micaceous  sandstone,   light  gray  and  of  fine  texture 215 

Gray  micaceous  sandy  shale    220 

Laminated,   dark  and  light  gray  micaceous  shale    225 

Gray,    stony    shale     230 

Elack  shale  and  some  gray  shale   245 

Gray  shaly  sandstone  with  infiltrated  lime    250 

Gray  sandstone   and   shale    255 

Gray   sandstone,    some   limestone    260 

Gray   sandy   shale,    some    limestone    265 

Gray  sandy  shale  and  concretionary  siderite,  some  limestone 270 

Dark  gray  shale    ' 275 

Gray  sandstone  and  yellowish  sandstone  with  infiltrated  lime 280 

Coarse    white    sandstone,    yellow    micaceous    sandstone    and    some 

gray    shale     ■ 285 

Coarse  white  sandstone  and  gray  shale    290 

White    sandstone,    some    micaceous    sandstone,    little    dark    shale 

and    limestone     295 

Gray  micaceous   sandy  shale,   some  gray  shale    300 

Gray  micaceous   sandy  shale    305 

Gray  micaceous   shale    310 

Gray  micaceous  shale,   some  fragments  of  limestone    320 

Dark  gray  shale,  few  bits  of  limestone   325 

Dark  gray  shale  and  a  few  fragments  of  limestone  and  siderite..  330 

Gray  shale,  siderite  concretion,  some  bits  of  limestone  and  pyrite.  .  335 

Dark  gray  and  black  shale    340 

Gray  shale,  limestone  and  siderite  concretions,  some  quartz  grains  345 
Gray   micaceous   sandy   shale    and    black   micaceous    shale,    a    few 

bits  of  limestone    : 350 

Gray   micaceous   sandy    shale    355 

Dark   gray  shale    360 

White   organic  limestone,   brecciated.   crinoid  stems.      Rhombooora, 

lepidodendroides,    ethyris,     (?),    and    fragments    of   other   brach- 

iopods    noted.       One    fragment    with    peculiar    finely    reticulate 

structure    noted    370 

Yellowish  gray  limestone,  organic  breccia 375 

Red  shale  and  gray  shale,  with  some  black  shale   380 

Fire  clay,  some  fragments,   of  coal  and  green   shale 385 

Greenish    gray    shaly    sandstone    390 

Like  the  preceding,  with  some  limestone    395 

Light   gray   micaceous    shale    400 

Light   gray  sandy   shale 405 

Dark   gray  stony   shale    410   ' 

Micaceous  sray  sandy  shale,  with  a  few  fragments  of  coai 425 

Micaceous  sandy  shale  and  shaly  sand,  laminated,  showing  shreds 

of    vegetation 430 

—4  Gr 


feet. 
To 
205 
210 
215 
220 
225 
230 
245 
250 
255 
260 
265 
270 
275 
280 


290 
295 

300 
305 
310 
320 
325 
330 
335 
340 
345 
350 

355 
360 
370 


375 
380 
385 
390 
395 
400 
405 
410 
425 
430 

435 


50                 OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,  [bull.  no.  22 

Logs — Continued. 

Depth  in  feet. 

From  To 

Laminated   sandstone,   shaly,   carbonaceous    435  440 

Micaceous  sandy  gray  shale,  with  bits  of  carbonaceous  shreds...  440  445 

Gray  shaly  sandstone  with  carbonaceous  laminae    445  450 

Dark  and  light  sandy  shale,  laminated    450  460 

Gray    shaly    sandstone,    coal    and    some    calcite    from    a    joint    in 

the  coal    460  465 

Greenish  gray  shaly  limestone  of  compact  texture    465  470 

Sandy  shale,   gray  and  yellow  limestone    470  475 

Gray  micaceous  sandstone,  with  some  limestone 475  480 

Sandstone  with  concretionary  impregnations  of  yellow  limestone..  480  485 

Dark,  almost  black,   stiff  shale    485  490 

Black    limestone,    organic    490  495 

Coal     495  500 

Black  shale,  with  imprints  of  leaves   500  505 

Coal,   some   shale    505  510 

Limestone  and  some  micaceous  shaly  sandstone    510  515 

Coarse    white    sandstone,    and   pyrite    and    some    white    brecciated 

limestone    515  520 

Micaceous  coarse  sand   520  525 

Micaceous,  coarse  sand,  with  some  gray  shale  and  limestone 525  530 

White  micaceous   sandstone    530  535 

White  micaceous  sand,   and  some  coal  and  limestone 535  540 

Dark  blotchy  brown  limestone,  with  chonetes,  productus,  Fusulina, 
Rhombopora,    Fistulipora,    crinoid    stems,    some    coal    and    some 

black   carbonaceous   shale    540  545 

Micaceous   and  carbonaceous  gray  shale    545  550 

Dark  blotchy  limestone   with   crinoid  joints 550  555 

Coal    555  560 

White  sandstone,  specked  with  minute  crystals  of  pyrite  and  some 

dark    shale     560  565 

White,  micaceous  and  pyritiferous  sandstone.     Some  black   "clod" 

with  Athyris  valve    565  570 

No    sample     570  575 

Gray  sandstone  with  concretions  of  siderite  and  limestone 575  580 

Gray  shale,  with  concretionary  material  as  in  preceding  sample.  .  .  580  585 

Dark   gray   shale 585  590 

Dark  gray  shale,   some  sand    590  595 

Black    shale     595  605 

Dark  shale  of  fine  texture    605  610 

Black   calcareous   stony   shale 610  615 

Black  shale  of  finest  texture    615  620 

Greenish  gray  shaly  sandstone,  with  pyrite  crystals   620  625 

Greenish  gray  shale,   sandy    625  630 

Gray    sandy    shale    and    fire    clay,    with    bituminous    films    in    thin 

joints     630  635 

Greenish  shale,  pyritiferous    635  640 

Light  greenish  gray  shale,   soapstone    640  645 

Gray  shale  and  micaceous  sandstone    645  650 

Sandstone,  gray,  soft    650  655 

Shaly,  micaceous  and  laminated  sandstone,  and  black  shale 655  660 

Dark  gray  sandy  shale    660  670 

Dark    shale    670  675 

Black  shale    675  680 

Laminated    sandy    shale     680  685 

Greenish   gray,   stony  shale 685  690 

Black    shale,    with    coal,    considerable    pyrite    and    frequent    frag- 
ments of  pyritized  woody  tissue   690  695 

Black  and   gray  shale,  stony  and  sandy    695  700 

Gray   sandy   shale    700  705 

Dark    shale   of   fine   texture    705  715 

Gray  sandy  rock,  with  some  coal,  some  pyrite  and  minute  spheri- 
cal concretions  of  siderite   715  720 

Black   carbonaceous   shale   and   coal,   some   dark   limestone.      Some 

pieces  of  coal  show  woody  structure   720  725 

Dark  limestone  and  black  shale,  crinoid  stems  and  pieces  of  pyrite  725  730 

Black    shale 730  735 

Dark  sandy  shale,   little  fire  clay  and  limestone    (yellow) 735  740 

Black   sandy   micaceous   shale    740  745 

Coal,  some  black  sandy  shale,  pyrite  showing  woody  structure.  .  .  .  745  750 

White  micaceous  sand,  coal  and  some  fire  clay   750  755 

No    sample     755  760 

White  sand,  bits  of  yellow  limestone 760  765 

Gray  sandstone,  some  yellow  limestone  and  black  shale   765  770 

Dark  gray  shale  and  limestone,  some  sandstone  and  bits  of  pyrite  770  775 

Black  shale,  some  dark  limestone  and  pyrite  fragments 775  780 

Black   shale,    some   pyrite    780  785 

Dark    gray   shale    785  790 

Gray  sandy  shale,  few  pieces  of  siderite  concretions 790  795 

Gray  sandstone  and  bits  of  siderite   795  800 

Gray  sandy  micaceous   shale    800  805 


BLATCHLET] 


CRAWFORD   COUNTY   LOGS. 


51 


Logs — Continued. 


White  micaceous  sandstone,  gray  micaceous  sandy  shale,  little 
limestone   and  oxidized  red  fragments 

White  micaceous  sandstone,  some  gray  sandy  shale,  and  oxidized 
fragments    

White  sandstone,  some  dark  shale   

White  sandstone,  some  dark  shale,   and  oxidized  red  material.... 

White  micaceous  sandstone,   some  dark  shale    

White   sandstone    

White  micaceous  sandstone,  with  a  little  gray  shale  and  oxidized 
red   material    

Dark  sandy  shale    

Black  micaceous  shale,  with  some  yellow  coarse  grained  sandstone 

Yellow  sandstone,  coarse  grained  and  some  black  shale   

Gray  sand,  little  black  micaceous  shale    

Black  micaceous  shale  and  some  gray  sand   


Depth  in 

feet. 

From 

To 

805 

810 

810 

815 

815 

825 

825 

830 

830 

835 

835 

840 

840 

845 

845 

850 

850 

855 

855 

860 

860 

870 

870 

885 

No.  8 .— C.  T.  Cochran,  No.  9. 

Location— NE.  corner  SW.  %  sec.  21,  Montgomery  Township. 
Elevation — Unknown. 

Depth  in  feet. 
From  To 

Yellow   sandstone,    disintegrated    1  6 

Yellow    sandstone     :  • •  •  •  •. 6  1Z 

Yellow  sandstone  with  infiltrated  lime   and  oxidized  siderite   con- 
cretions     

Yellow  sandstone,   and  sandstone  concretions    19  24 

Yellow   sandstone,    siderite    concretions,    and   some   black   crinoidal 

limestone     24  38 

Yellow  sand,  dark  calcareous  limestone  and  siderite  concretions.  .  38  45 
Brown    coarse     sandstone,     dark    limestone,     siderite    concretions, 

spherical,  one-half  inch  in  diameter 45  51 

Gray  sandstone  with  infiltrated  lime  and  siderite  concretions 51  58 

Gray  sandstone  with  infiltrated  lime,  and  siderite  concretions....  58  64 

Dark   gray  shale    64  78 

Black    shale     78  85 

Gray  micaceous  sandy  shale    85  91 

Gray  micaceous   shaly  sandstone    91  98 

Gray    shale    98  104 

Gray  shale,  siderite,  a  few  fragments  of  coal    104  111 

Gray  shale  and  siderite    Ill  117 

Black    shale    117  124 

Gray  sandy  shale,  fragments  of  coal   124  130 

Gray  micaceous   shale    130  137 

Fine   gray  laminated  sandstone,    black   shale    137  143 

Gray   sandstone,   black   shale   and   brown   limestone 143  150 

Gray  sandstone,  brown  limestone  and  black  shale    150  156 

Brown  limestone,  gray  shale  and  gray  sandstone    156  163 

Gray  shale,  gray  sandstone,  and  fragments  of  siderite  concretions  163  170 

Gray  laminated  micaceous  sandstone,   and  siderite   concretions...  170  176 

Coarse   gray  micaceous   sandstone    176  223 

Coarse    gray    micaceous    sandstone,    a   few    pieces    of    coal,    pyrite 

and    siderite    223  231 

Coarse   gray  micaceous   sandstone,   with  infiltrated  lime 231  237 

Coarse  gray  micaceous   sandstone  with   infiltrated  lime   and   frag- 
ments of  black  shale    237  244 

Coarse  gray  micaceous  sandstone  with  infiltrated  lime,   and  frag- 
ments of  impure  coal    244  250 

Gray  shaly  sandstone,  and  concretions  of  brown  limestone 250  257 

Gray  sandy  shale    257  270 

Greenish  gray  shale  with  infiltrated  lime    270  276 

Gray    micaceous    sandstone    276  296 

Coarse   gray  sand    296  309 

Coarse  gray  sand  with  carbonaceous  folia    309  315 

Coarse  gray  sand    315  328 

Coal  and  fire  clay,  a  few  fragments  of  mottled  limestone 328  335 

Gray   sandstone 335  341 

Gray   sandstone  and   limestone    341  348 

Gray   calcareous   limestone    348  361 

Greenish  gray  sandstone  and  gray  calcareous  limestone    361  367 

Gray  shale  and  calcareous  limestone    367  374 

Gray  micaceous  shale,  with  some  gray  calcareous  limestone 374  380 

Gray  micaceous  sandstone  and  gray  shale    380  387 

Gray   shale    387       .    413 

Gray  sandy   shale    413  419 

Gray  sandy  micaceous   shale    419  432 

ilttRAk 


a  i  i^v  «*  *-  inoi. 


52 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


Logs — Concluded. 


Depth  in  feet. 

From  To 

Coarse   gray  sandstone  with   carbonaceous  folia    432  439 

Gray    shale    439  445 

Gray    shale,    micaceous    445  452 

Coal,  siderite  concretions,  pyrite  crystals  and  a  few  white  gypsum 

crystals     452  465 

Gray  micaceous   shaly   sandstone    465  471 

Gray  micaceous  sandstone  with  infiltrated  lime    471  478 

Gray  shale,   gray  sandstone    478  497 

Coal,   gray  shale,  dark  limestone,  pyrite  and  a  few  crinoid  stems 

noted    497  504 

Coal,  pyrite,  and  a  few  crinoid  stems  noted   504  510 

Coarse  gray  micaceous  sandstone  with  infiltrated  lime 510  523 

Coarse  gray  micaceous   sand    523  530 

Gray  micaceous  sandy  shale    530  536 

Gray  shale,  fragments  of  coal  and  pyrite    536  543 

Black  shale,  some  limestone,  and  numerous  crinoid  stems  noted..  543  549 

Gray  micaceous  sandstone    549  556 

Dark    limestone    with    Chonetes    punctatus.      Rhombopora    lepido- 
dendroides  and  showing  some  intensely  green  specks.     Presence 

of  Fusulina  uncertain    '. 556  562 

Coal,   some   limestone    562  569 

Gray   sandy   shale,   some   pyrite    569  575 

Gray  sandy  micaceous  shale    575  582 

Coarse  gray  sand  with  fragments  of  black  shale 582  588 

Gray  sandstone  with   some  limestone    588  595 

Gray  shaly   sandstone    595  608 

Gray  shale  and  sandstone    608  621 

Gray    shale    621  666 

Black  and  gray  shale    666  673 

Black  shale    673  679 

Brown  limestone,  greenish  and  reddish,  dolomitic,  shaly  limestone, 

and  black  gray  shale    679  686 

Gray  limestone,    some   gray   shale   and  fragments   of   brown   lime- 
stone,   two   small   gasteropods    686  692 

Coal,    some   gray  and  and   brown   limestone    692  699 

Gray  sandy  micaceous  shale    699  705 

Gray    shale    705  712 

Gray  sandy  micaceous  shale    712  725 

Gray    shale 725  731 

Black    shale 731  737 

Black   and   gray   shale    737  743 

Black    stiff    shale     743  750 

Coal,    some    gray   shale    750  756 

Coarse    gray    sandstone   with    infiltrated   lime,    fragments    of   coal, 

and  gray  shale    756  763 

Gray  sandy  micaceous  shale 763  769 

Black  shale,  coarse  gray  sandstone,  fragments  of  coal 769  775 

Gray  sandy  shale,   black  shale    775  781 

Gray  micaceous  shale,  gray  sandstone  with  infiltrated  lime 781  787 

Gray  shale  and  gray  micaceous  shale    787  793 

Gray    shale     793  806 

Black   stiff   shale    806  813 

Coal,   and   fire   clay    813  820 

Gray   shale    820  834 

Gray  micaceous   sand  and  shale    83  4  840 

Yellow    micaceous    sand     840  846 

Gray   shale    846  862 

Gray  shale  with   fragments  of  gray   sandstone    862  873 

Gray   and   black   shale    873  884 

Black    shale     884  895 

Gray    shale    895  906 

Grav   sandstone   with   shreds   of  vegetation    and   a  few   fragments 

of   coal    906  912 

Gray  sandstone  with  shreds  of  vegetation    912  923 

Gray  micaceous  sandstone    923  928 

White  micaceous  sand  with  fragments  of  shale   928  934 

Gray   laminated   sandstone    934  940 

Gray  laminated  sandstone,  brown  sandstone   940  952 

Brown  sandstone   (note  on  sack  "Oil  952  to  973"),  gray  sandstone  952  958 

Brown  sandstone,  some  gray  sandstone    958  964 

Brown  sandstone,   some  gray  sandstone,   pyrite    964  970 

Brown   sandstone,    some   gray   sand    970  975 

Stratigraphy. 

Pleistocene. 

The  records  in  Plate  II  give  an  idea  of  the  difference  in  thickness  of 

the  drift  overlying  the  hard  rocks.     Some  records  show  it  to  be  thin,  due 


blatchley]  PENNSYLVANIA^   FORMATIONS.  53 

to  conditions  of  erosion  and  deposition.  The  drift,  measures  from  25 
to  110  feet  in  the  examined  logs;  while  a  number  of  logs  over  the  field 
show  an  average  of  75  feet  to  the  bed  rock,  on  which  the  drive-pipe  is 
set. 

Pennsylvania™. 

The  Pennsylvanian  or  "Coal  Measures"  rocks  are  separable  into  three 
divisions;  an  upper  part,  the  McLeansboro  formation,  middle  part,  the 
Carbondale  formation,  and  a  basal  part,  the  Pottsville  formation. 

McLeansboro  Formation — The  rocks  of  the  McLeansboro  formation 
lie  between  the  top  of  Herrin  (No.  6)  coal  and  bed  rock  near  the  sur- 
face. From  measurements  and  estimates  of  logs  in  the  section  the  aver- 
age thickness  of  the  formation  is  found  to  be  about  485  feet.  Shales 
and  sandstones  dominate  in  this  division  and  are  accompanied  by  several 
streaks  of  limestone  and  many  coals.  One  well  reports  seven  beds  of 
coal.  The  most  conspicuous  bed  of  these  rocks  is  the  limestone  used  as 
a  key  line  in  the  section.  Dr.  Udden  describes  it  as  a  dark  limestone 
containing  Fusulina  fossils.  All  of  the  records  show  notations  of 
Fusulina  except  Nos.  2  and  3.  The  position  of  the  bed  is  estimated 
in  No.  2  by  comparison  with  No.  1  and  is  thought  to  lie  at  a  depth 
of  about  560  feet.  The  black  limestone  at  490  feet  in  No.  3,  al- 
though no  Fusulina  are  reported,  seems  to  correlate  with  other  logs 
of  the  section  and  is  designated  as  that  horizon.  An  effort  is  being  made 
by  geologists  to  determine  this  bed  over  Illinois  by  its  fossils  and  thus 
procure  a  definite  marker  for  the  Herrin  (No.  6)  coal  immediately 
underneath. 

The  two  limestones  noted  at  200  and  300  feet  by  Dr.  Udden,  in  well 
No.  2,  page  35;  and  alluded  to  as  possibly  equivalent  to  the  limestone 
160  feet  above  No.  6  coal  at  Belleville  and  the  Carlinville  limestone, 
suggest  their  possible  correlations  through  the  columnar  section.  The 
interval  between  the  two  limestones  is  about  130  feet.  The  interval  be- 
tween the  upper  or  Carlinville  (?)  limestone  and  the  "Fusulina"  lime- 
stone is  about  365  feet  and  the  interval  between  the  lower  limestone 
and  the  key  bed  is  about  220  feet.  In  other  sections  of  the  State,  the 
Carlinville  limestone  is  about  250  feet  above  the  overlying  limestone 
of  the  Herrin  coal.  The  red  shale  spoken  of  elsewhere  as  lying  in  the 
McLeansboro  is  reported  only  in  logs  No.  4  and  7  at  depths  of  270  and 
380  feet  respectively.  The  intervals  between  the  red  bed  and  the 
"Fusulina"  limestone  are  respectively  210  and  160  feet. 

Carbondale  Formation — The  rocks  of  the  Carbondale  formation  lie 
between  the  tops  of  Herrin  (No.  6)  and  Murphysboro  (No.  2)  coals. 
The  Herrin  coal  is  the  first  beneath  the  "Fusulina"  limestone.  The 
Murphysboro  coal  lies  above  the  Pottsville  sandstones  and  is  usually 
separated  from  these  by  shales  or  a  thin  limestone.  The  Carbondale 
formation  is  mostly  shale,  with  sandy  shales  at  the  bottom.  There  are 
either  three  or  four  coals  noted  in  each  record.  The  columnar  section 
shows  much  irregularity  between  the  Herrin  and  the  lowest  coal.  The 
thickness  of  the  division  varies  from  200  to  450  feet.  Logs  1,  2,  3,  7 
and  8  show  an  average  interval  of  310  feet  between  the  Herrin  coal  and 
the  Pottsville.  In  type  localities  of  other  sections  of  Illinois,  the  inter- 
val is  between  300  and  350  feet. 


54  OIL  FIELDS  OF  CKAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

Pottsville  Formation — The  Pottsville  rocks  are  the  lowest  members 
of  the  Pennsylvania!!  and  are  essentially  coarse  sandstones  merging  into 
sandy  shales  at  the  top  and  occasionally  split  with  lenses  of  shale.  The 
lower  portions  of  the  records  used  in  the  columnar  section  are  pre- 
dominantly sandstones  and  in  position  correspond  with  Pottsville  beds. 
These  rocks  lie  below  the  Murphysboro  (No.  2)  coal.  The  sandstone 
at  the  base  of  the  sections  is  known  as  the  Eobinson  sand.  There  are 
as  many  as  four  distinct  lenses  of  this  sand  interbedded  with  shale.  The 
upper  portion  of  the  sand  rocks  are  oil-bearing  but  lower  down  they  yield 
much  salt  water. 

Lawrence  County. 

The  explored  rocks  of  Lawrence  County  lie  in  the  Pennsylvanian  and. 
Mississippian  series.  These  major  divisions  are  overlain  with  unequal 
thicknesses  of  drift.  The  Pennsylvanian  rocks  are  from  800  to  1,300 
feet  thick.  This  great  variation  in  thickness  is  due  to  the  unconformity 
at  the  top  of  the  Mississippian,  accentuated  by  preexisting  structure  and 
preglacial  erosion.  The  Mississippian  rocks  are  not  completely  pene- 
trated but  they  have  been  well  explored  to  a  depth  of  475  feet  below 
their  top. 

The  columnar  section,  Plate  IIIA,  is  made  up  of  logs  from  all  sections 
of  Lawrence  county.  They  are  plotted  in  order  from  south  to  north. 
The  top  of  the  wide-spread  Ste.  Genevieve  limestone,  known  locally  as  the 
McClosky  sand,  is  used  as  a  key  bed  through  the  columnar  section.  All 
records  are  plotted  with  respect  to  this  line.  The  section  is  made  up  of 
the  following  records,  which  correspond  by  number  to  those  printed  on 
Plate  3. 

LOGS. 

NO.  1. 

Operators — Snowden  Bros. 
Farm  and  well — Laughlin,  No.  1. 
Location— SE.  %  sec.  32,  Lukin  Township. 
Elevation— 469  feet. 

Thickness  Depth 

Feet  Feet 

Sand  and  clay,  yellow,   soft    20  20 

Slate,    white     15  35 

Limestone    shell     3  38 

Slate,    white     7  45 

Limestone     shell     48 

Slate,    white     12  60 

Sand,    loose,     (water)     '. 9  69 

Slate,    white    66  135 

Limestone    shells 5  140 

Shale,    black    •.  .  .  40  180 

Limestone    shell     •. 2  182 

Slate,    black,    loose    18  200 

Limestone  shell,  white    4  204 

Slate    56  260 

Sand,  white  loose    (hole  full  of  water,   290  feet) 30  290 

Limestone     21  311 

Slate,   black  and  white    89  400 

Limestone  shell,  white    4  404 

Sandy   limestone,    white,    (water,    410    feet)     6  410 

Limestone  shell,  white    12  422 

Slate,    black    5  427 

Limestone    shell,    gray    11  438 

Red   rock    7  445 

Slate,    white    55  500 

Shale  and  slate,  black 105  605 


55 


)th 
et 
.26 
32 

;90 
;93 

10 
30 

'80 
'82 

;30 

172 

177 

180 

!85 

140 

145 

180 

)76 

>86 

(96 

.25 

.56 

.80 

!15 

!35 

!00 

',04 

115 

!38 

545 

140 

150 

506 

514 

514 

'32 

T45 

750 

T75 

?32 

?50 

565 

*70 

?75 

*95 

)00 

)20 

)30 

)85 

)00 

)12 

330 

LOO 

L30 

L52 

L56 

160 

165 

165 


Of 

>et. 
To 

5 
20 

25 

35 
40 


54 


of 
sa 
lo 
dc 
T 
at 
as 
u] 
m 


5LATCHLEY] 


LAWRENCE    COUNTY   LOGS. 


Logs — Continued. 


3andy   slate,   white 

limestone   shell •" 

Shale,    brown    

Liimestone    shell    

Slate,    white 

Shale,    brown,    hard 

Slate,  white,   soft    

Limestone    shell,    white    

Slate,    white    

3and,  white,    (salt  water,   830  feet)    

Broken  lime,  black,  loose    

Shale,    black    

Limestone  shell,  white   

Slate,    black,    soft    

Sand,    brown,    bridged    

Slate,    white    

Slate  and  shale,  black    

Limestone   and  sand,    (water,   1,086    feet)     

Shale,    black    

Limestone,    white    

Slate,    black     

Sand  and  broken  limestone,  white,   soft    

Sandy  slate,   white    

Slate,  white,  soft    

Sandy   shale    

Limestone,   white,    hard    

Sand,    white,    soft    

Sandy   clay,   brown    

Limestone,    white     

Slate,   black    

Limestone,    white     

Slate,  white,  soft    

Sand,  brown,    (show  of  oil,  1,506  to  1,514  feet) 

Limestone,   white    

Sand,    (water)    (show  of  oil,  1,705  to  1,732  feet) 

Limestone     

Slate    

Sand,    (hole  full  of  water,   1,775   feet)    

Slate     

Limestone     

Slate 

Red    rock     

Limestone    shell    

Slate     

Limestone     

Slate     

Red    rock    

Slate     

Sand,    (oil   show,   1,985   to   2,000  feet)    

Shale,    hard,    black    

Slate     

Limestone     

Slate     

Limestone      

Sand,    (show  of  oil)    

Slate     

Limestone     

Total   depth    


55 


Feet 


less 

Depth 

t 

Feet 

21 

626 

6 

632 

58 

690 

3 

693 

17* 

710 

20 

730 

50 

•  780 

2 

:  782 

48 

830 

42 

872 

5 

877 

3 

880 

5 

885 

55 

940 

5 

945 

35 

"  080 

96 

1.076 

10 

1,086 

10 

1,096 

29 

1,125 

31 

1,156 

24 

1,180 

35 

1,215 

20 

1,235 

65 

1,300 

4 

1.304 

11 

1,315 

23 

1,338 

7 

1,345 

95 

1,440 

10 

1,450 

56 

1,506 

8 

1,514 

100 

1,614 

118 

1,732 

13 

1,745 

5 

1,750 

25 

1,775 

57 

1,832 

18 

1,850 

15 

1,865 

5 

1,870 

5 

1,875 

20 

1,895 

5 

1,900 

20 

1,920 

10 

1,930 

55 

1,985 

15 

2,000 

12 

2.012 

18 

2,030 

70 

2,100 

30 

2,130 

22 

2,152 

4 

2,156 

4 

2,160 

5 

2,165 

2,165 


No.  2. 

Operators — Ohio  Oil  Company. 
Farm  and  well — W.  H.  Snyder,  No.  7. 
Location — SW.  %  NW.  %  sec.  25,  Dennison  Township. 
Elevation — 495  feet. 

(This  record  was  compiled  by  Dr.  J.  A.  Udden  from  an  examination  of 
well  samples.) 


Loess    

Loess,    silty 

Gray  sandy  limestone  and  micaceous  and  calcareous  sand.  Spher- 
ules of  pyrite  noted,  measuring  from  14  to  1  mm.  in  diameter. . 

Micaceous  gray  sandstone  with  occasional  shreds  of  carbonaceous 
material     

Sandy    shale 


Depth  in 
From 

feet. 
To 

1 

5 

5 
20 

20 

25 

25 
35 

35 
40 

Depth  in 
From 

feet. 
To 

40 

45 

45 
50 

50 
55 

5G  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.      [bull.  no.  22 

Lags — Continued. 


Gray    shale 

Gray  sandstone,  coal,  black  shale  and  pieces  of  gray  limestone. 
There  were  crinoid  stems,  one  crinoid  plate  from  a  calyx  and  an 
umbo  of  a  small  brachiopod 

Light  gray  shale  of  fine  texture.     No  effervescence 

Gray  calcareous  and  sandy  rock,  with  much  concretionary  calcare- 
ous material.  One  large  fragment  was  black  concretionary 
limestone  with  imbedded  minute  white  shells  and  tubes,  appar- 
ently small   gasteropods   or   formanifera    55  60 

Shaly  sandstone,  some  shale,  white  and  yellow  limestone  of  con- 
cretionary  appearance,    and    some    coal 

Sandy  shale  of  very  light  gray  color 

Dark    gray    micaceous    shale 

Dark  shale  and  black  shale,  fragments  of  concretionary  limestone, 
Nucula  beyrichi  ( ?)  crinoid  stems,  tubes  of  Ammodiscus,  and 
fragments    of   concretionary   limestone 

Black    shale 

Black  shale,  black  calcareous  "clod,"  occasional  pieces  of  coal, 
crinoid  stems,  "mineral  charcoal"  showing  woody  structure, 
pyrite    and    calcite 

Gray   sandy   micaceous    shale 

Gray    micaceous    sandstone 

Gray  sandy  shale,  black  shale  and  coal,  with  some  calcareous 
material 

Gray  sandy  and  micaceous  shale 

Fine    gray    sand. 

Fine   gray   shaly   sand 

Fine  gray  shaly  sand  with  dark  shaly  laminae 

Laminated    shaly    sandstone 

Laminated    gray    sandy    shale 

Dark  micaceous  and  sandy  shale 

Dark    shale,    micaceous 

Sandy  shale  and  sandstone 

Coarse,  micaceous  gray  sand 

Micaceous  gray  shale 

Dark  shale  of  fine  texture 

Dark  shale,  black  shale,  some  sandstone,  impure  coal,  and  frag- 
ments of  limestone,  yellow.  Crinoid  stems  and  a  small  gas- 
teropod    noted , 230  235 

Fire  clay,  sandy  shale,  and  concretionary  yellow  limestone,  which 
is  fossil-bearing.     A  few  fragments  of  coal  noted 

Gray     shale 

Gray   stony   shale 

Dark  micaceous   shale 

Gray   micaceous   shale 

Dark   micaceous    shale 

Gray  shaly  sandstone  and  sandy  shale 

Gray  micaceous  sand  of  fine  texture ^ 

Gray  sand  and  some  lumps  of  light  fire  clay  or  shale  containing 
imprints    of    leaves 

Clean  and  white  micaceous   sand 

Gray   micaceous   sandstone 

Light  gray  fire  clay,  coal,   some  sandstone,  and  a  little  limestone. 

Minute   spherules  of  siderite  present  in   the  fire   clay 335  340 

Cream-white  limestone  of  fine  granular  homogeneous  texture,  with 
occasional  minute  green  specks,  and  occasional  indistinct  organic 
fragments     

White  limestone  of  fine  uniform  texture.  Some  fragments  show  a 
fine  reticutale,  clastic  (?)  structure.  Some  greenish  shale  and 
pyrite     • 

Brownish  red  marly  clay  and  limestone 

Red  marl,  greenish  marl,   and  white  limestone 

White   limestone   of   fine   uniform   texture,   with   a   few   fragments 

of   gray   shaly  limestone    360  365 

Gray   sandstone,    biotitic   and    impregnated   with   irregular   kernels 

and  layers  of  yellow  limestone 365  370 

Some  sandstone,  some  white  limestone,  yellow  lime  and  some  frag- 
ments of  a  slowly  effervescing  material 370  375 

Dirty  dark  marl  and  limestone,  with  some  fragments  of  bright  red 
marl,   and   some  black   fragments 

Grav    sandstone 

Very  dark  shaly  sandstone,  bituminous  and  green  shale 

Dark,  almost  biack,  sandy  micaceous  shale 

Dark  £ray  shale  of  fine  texture 

Gray  micaceous  shaly  sandstone   and  some  white  limestone 

Dark  gray  shale  of  fine  texture,   coal    

Dark  gray  shale  of  fine  texture  and  some  white  limestone 

Gray  micaceous   laminated   sandstone 


60 

65 

65 

70 

70 

90 

90 

100 

100 

105 

105 

110 

110 

120 

120 

140 

140 

145 

145 

155 

155 

165 

165 

170 

170 

175 

175 

180 

180 

185 

185 

195 

195 

200 

200 

205 

205 

215 

215 

225 

225 

230 

235 

240 

240 

245 

245 

250 

250 

255 

255 

260 

260 

265 

265 

270 

270 

310 

310 

315 

315 

320 

320 

335 

340  345 


345 

350 

350 

355 

355 

360 

375 

380 

380 

385 

385 

390 

390 

400 

400 

405 

405 

410 

410 

415 

415 

425 

425 

430 

feLATOHLEY]                                LAWRENCE    COUNTY   LOGS.  57 

Logs — Continued. 

Depth  in  feet. 
From  To 

Dark  gray  shale  and  some  brown  clay 430  435 

Dark  gray  sandstone  with  layers  of  carbonate  of  iron 435  440 

Dark  gray  micaceous  shale,  and  dark  gray  sandstone  with  layers 

of  carbonate  of  iron 440  445 

Dark  gray  micaceous  shale  ;   dark  gray  sandstone  with  layers  of 

carbonate  of  lime,  and  a  few  fragments  of  limestone 445  450 

Dark  gray  shale,   siderite   and  pyrite 450  455 

Dark  gray  shale  of  fine  texture  and  some  siderite 455  460 

Dark   gray   micaceous   shale,    and   gray   sandstone   with   layers   of 

carbonate    of    iron 460  470 

Dark  gray  shale,  sandstone,  and  sandstone  with  carbonate  of  iron  470  475 

Dark  gray  shale  of  fine  texture  and  some  siderite 475  480 

Dark  gray  micaceous  shale,   and  some   siderite 480  485 

Dark  gray  shale,  dark  micaceous  shale,  and  siderite 485  495 

Dark  gray  shale,  white  and  dark  limestone 495  500 

Siderite  concretions  showing  cracks  filled  with  calcite,  gray  lime- 
stone   and    shale 500  505 

Gray  shaly  sandstone,  siderite  concretions  and  some  gray  lime- 
stone      505  510 

Gray  shaly  sandstone,  fragments  of  white  and  gray  limestone 510  515 

Gray  sandy  shale,   siderite  and  fragments  of  gray   limestone 515  520 

Dark  gray  shale,  some  greenish  shale,  siderite,   and  fragments  of 

gray    limestone 520  525 

Dark  gray  micaceous  shale,  and  some  siderite 525  530 

Dark  gray  shale,  some  greenish  shale  and  some  siderite 530  535 

Dark  shale,   siderite   and   some   brown  limestone 535  540 

Dark    shale,    siderite,    fragments    of    limestone,    and    a    part    of    a 

crinoid    stem    noted 540  545 

Dark  shale  and  fragments  of  limestone 545  560 

Black  shale  with  organic  calcareous  fragments.  Crinoid  stems 
and  Rhombopora  lepidodendroides   noted.      Spherules   of  siderite 

present.      Spines   of   Productus    (?) 560  565 

Black  shale  with  organic  calcareous  material,  limestone,  frag- 
ments of  gray  micaceous  sandstone,  numerous  crinoid  stems 
noted,  also  siderite.  Hustedis,  Chonetes  punctatus,  Rhombo- 
pora lepidodendroides,   gasteropods  and  crinoid  stems  noted,   as 

also    spines   of   Productus    (?) 565  570 

Black  shale  with  calcareous  material,  fragments  of  limestone  and 
sandstone,     small     gasteropods,     numerous     crinoid     stems,     and 

spines    of   producti    noted 570  575 

Coal,    gray   shale,    limestone,    numerous    crinoid    stems    and   pyrite 

noted 575  580 

Brownish    dark    limestone,    gray    shale,    and    fragments    of    coal. 

Considerable  pyrite,   fossil  wood  in   fragments 580  585 

Brownish    dark    limestone,    gray    shale,    some    crinoid    stems    and 

Chonetes    noted 585  590 

Gray    micaceous    shale,    gray    shale,    gray    limestone    and    brown 

limestone    590  595 

Gray  sandy  shale,  fragments  of  brown  and  gray  limestone 595  600 

Dark  gray  shale  of  a  fine  texture  and  some  pyrite 600  605 

Dark  gray   shale   of   a   fine   texture,    some   gray   micaceous   shale, 

pyrite  and  fragments  of  coal •  605  610 

Dark  gray  shale  of  a  fine  texture 610  620 

Dark    gray    micaceous    shale 620  625 

Dark  gray  shale  and  fragments  of  limestone 625  630 

Dark  gray  micaceous  shale  and  some  pyrite 630  635 

Dark  gray  shale,  fragments  of  coal  and  limestone 635  640 

Dark  gray  shale,  fragments  of  limestone  and  some  pyrite 640  645 

Light    gray    sandstone    of    fine    texture,    and    fragments    of    black 

shale     645  650 

Light  gray  sandstone,  and  some  fragments  of  black  shale 650  660 

Dark  gray  shale  and  light  gray  sandstone 660  665 

Light   gray   micaceous   fine    sand 665  680 

Fine  white  micaceous  sand  with  infiltrated  lime 680  685 

Fine  white  micaceous  sand  and  some  dark  gray  shale 685  695 

Fine  gray  micaceous  sand  with  infiltrated,  lime 695  700 

Dark  gray  shale  and  gray  sandstone 700  705 

Gray    micaceous    laminated    sandstone 705  710 

Coai,   some  gray  shale,  and  a  few  fragments  of  limestone 710  715 

Gray  micaceous  laminated  sandstone  and  some  coal 715  720 

Micaceous    sandstone 720  725 

Dark    grav    shale 725  730 

Black  shale  of  fine  texture 730  735 

Very  dark   stony   shale   of   fine   texture 735  740 

Gray   micaceous    sandstone,    some    black    shale    and    fragments    of 

white    limestone 740  745 

Gray  micaceous  sandstone,  soft  and  containing  calcareous  mate- 
rial       745  750 


58  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.       [bull.  no.  22 

Logs — Continued. 

Depth  in  feet. 
From  To 

Micaceous    sandstone 750  755 

Dark  shale,  sandstone,  coal,  with  some  limestone  fragment's'.'...'.'.  755  760 

Fire  clay,   black  shale,  coal,  sandstone,   a  few  fragments  of  lime- 
stone,  yellow  siderite,   spherical  concretions,   measuring  from   V8 

to   2   mm.   in   diameter 760  770 

Dark   shaly   clay   and   micaceous   clay,   with   coal,    sandstone','  and 

small    spherical    concretions    of    siderite 770  775 

Dark  clayey  shale  and  some  micaceous  and  sandy  shale ...  775  780 

Gray  clayey  shale  of  fine  texture  with  some  stony  and  micaceous 

shale    7g0  790 

Dark   gray   shale,    in   part   sandy,   in   part   of   fine   texture.      Much 

pyrite,  some  pyritized  wood  coal  and  "mineral  charcoal" 790  795 

Light  gray  shale  or  fire  clay 795  800 

Light  gray   fire   clay,   white   sandstone,    coal   and   some   fragments 

of  white   and   yellow   limestone 800  805 

Gray  clay  shale  or  fire  clay,  coal,  and  white  sandstone 805  810 

Fire  clay,  sandy  gray  shale,  black  shale,  coal  and  brown  siderite..  810  815 

Soft  gray  micaceous  sandstone,  with  thin  carbonaceous  laminae 
black    shale,    brown    siderite,    pyrite    and    some    fragments    of 

fissured  white   limestone 815  820 

Black  shale  containing  calcareous  organic  fragments,  and  gray 
sandstone  containing  thin  layers   of   shaly  material,   pyrite   and 

spherules  of  gray  lime  measuring  about  y2  mm.  in  diameter 820  825 

Dark  shale  and  greenish  gray  sandy  fire  clay 825  830 

Gray  micaceous   sandstone,    fire  clay  and  black   shale  with  white 

limestone.      Crinoid   stems   noted 830  840 

Black    shale    and   gray   micaceous    sandstone,    brown    siderite    and 

white  limestone  and  partly  pyritized  mineral  charcoal 840  845 

Gray  micaceous  sandstone,    laminated,   gray  marly   shale 845  850 

Laminated    dark   shale   and   sandstone,    with   a    few   fragments    of 

coal,   apparently  from  thin   seam  in  rock 850  855 

Gray  sandstone   and   sandy   shale,   with   black   shale,    impure   coal 

and    siderite 855  860 

Like  the  preceding  but  with  some  pure  coal 860  865 

Gray  shale,  fire  clay,  gray  sandstone,  and  coaly  black  shale 865  S70 

Fire  clay,  gray  shale,  coal,  brown  siderite,  white  limestone,  frag- 
ments  of   shells   and   crinoid    stems,    pyrite    giving   an   oily    film 

on  the  water  when  washed 870  875 

Gray  clayey  shale,   and  coal,   with   some   calcareous  material 875  880 

Like  the  preceding.     Crinoid  joints  noted 880  885 

Gray  clayey  shale,  containing  fragments  of  coal  and  of  limestone, 

and  also  some  mica 885  900 

Mostly  fire  clay,  greenish  gray,  some  gray  sandstone,  black  shale, 
a  little  coal,   and  much  pyrite.     Fragments  of  shells  and  of 
limestone    noted.      In    the    fire    clay    a    joint    was    filled    with    a 

thin  film  of  black  bituminous  or  carbonaceous  material 900  905 

Gray   laminated   micaceous   sandstone 905  915 

Dark  gray,  sandy  and  micaceous  shale 915  920 

Gray  micaceous  sandstone  and  dark  shale 920  925 

Gray    sandstone,    greenish    fire    clay    and    coaly    black    laminated 

shale    925  930 

Gray    laminated    sandstone,    black    shale,    some    pieces    of    acreous 

shale,  brown   siderite.   fragments  of  white  limestone 930  935 

Sandstone,  from  dark  to  light  gray,  and  showing  streaks  of  car- 
bonaceous material,  together  with  black  coaly  shale 935  940 

Greenish  gray  fire  clay,  containing  spherules  of  fire  clay  from 
*/i  to  y2  mm.  in  diameter,  and  having  thin  joints  filled  with 
bituminous    or    carbonaceous    material.       Some    sandstone    and 

shale    noted 940  945 

Greenish  gray  fire  clay,  with  fractures 945  950 

Dark  shale  of  fine  texture 950  955 

Gray   coarse  sand  with   a   faint   odor   of  petroleum.      It   floats   on 

water    955  960 

Black  and  dark  shale,  with  some  carbonaceous  layers 960  965 

Dark  and  black  shale  and  concretionary  siderite  and  white  lime- 
stone      965  970 

Minutely  black  and  light  gray  limestone 970  975 

Minutely  blotched  dark  gray  limestone  and  some  dark  shale 975  980 

Dark    clayey    shale 980  900 

Black  shale  and  gray  sandstone 990  995 

Black  coaly  shale  with  brownish  streak  and  containing  streaks 
of  brown  flaky  siderite,  greenish  gray  fire  clay,   gray  limestone 

and  stony  fire  clay  filled  with  minute  spherules   of  siderite 995         1,000 

Black  and  gray  shale  and  a  fragment  of  coal 1,000         1,005 

Coarse   quartz   sandstone  with   fragments   of   siderite 1,005         1,010 

Gray    sandstone    with    siderite    grains 1,010         1,015 

Gray  sandstone  with  many  grains  of  brown  siderite 1,015         1,020 

Fairly   coarse    gray   sand 1,020         1,030 

Fine  gray  sand  having  the  odor  of  petroleum 1,030         1,035 


blatchlet]                                LAWRENCE    COUNTY   LOGS.  .      59 

Logs — Continued. 

Depth  in  feet. 
From  To 
Fine    gray    and    with    some    black    and    gray    shale,    white    lime- 
stone,   some   yellow   and   brown    siderite 1,035  1,040 

Gray  sandstone,  some  coarse  with  black  and  brown  grains,   some 

laminated,  alternating  with  black  micaceous  shale 1,040  1,045 

Black  shale,  some  sandstone,   and  some  white  limestone 1,045  1,050 

Black  stiff  shale,  some  clayey  shale  and  white  limestone 1,050  1,060 

Black  shale  and  fire  clay  with  a  few  fragments  of  coal 1,060  1,065 

Black  shale,  and  some  white  limestone 1,065  1,075 

Black  shale,  some  pyrite  and  white  limestone 1,075  1,080 

Black   shale   and   some   pyrite 1,080  1,085 

Gray   sandstone  with   imbedded   siderite   spherules   and   shreds   of 

carbonaceous    material 1,085  1,090 

Gray  sandstone  of  fine  texture 1,090  1,100 

Gray  sandstone  of  fine  texture  with  some  dark  gray  shale 1,100  1,105 

Gray    sandstone    of   fine    texture 1,105  1,110 

Gray  sandstone  with  some  fragments  of  white  limestone 1,110  1,115 

Laminated    shaly   sandstone,    consisting   of    layers    of    dark    sandy 

shale   and   light   gray   sandstone 1,115  1,120 

Laminated   sandstone  and   shale 1,120  1,130 

Green  and  black  fire  clay  of  fine  texture  and  cut  by  joints.. 1,130  1,140 

Greenish  blotchy  very  dark  fire   clay,  with  siderite   concretions  in 

large  fragments,  and  some  very  red  clay  lumps  with  green  core  1,140  1,145 

"Very  dark,  almost  black,   fire  clay 1,145  1,150 

Very    dark,    almost    black,    fire    clay,    or    a    greenish    tinge,    some 

bright   red   clay   showing   green    streaks,    some   white    limestone 

and  some  coal   or  bituminous   substance 1,150  1,155 

Very  dark  fire   clay 1,155  1,160 

Dark    fire-clay-like    shale 1,160  1,165 

Black  stiff  shale  and  fragments  of  siderite  concretions 1,165  1,170 

Black  shale  and  dark  green  shale 1,170  1,185 

Black    shale    and    gray    shale,    with    some    white    sandstone    and 

fragments    of    siderite    concretions 1,185  1,190 

Black    shale 1,190  1,195 

Black  shale  with  some  fragments  of  siderite 1,195  1,200 

Dark  gray  shale  of  fine  clay-like  texture 1,200  1,205 

Laminated  white  and  black  sandstone.     The  laminae  are  thin....  1,205  1,215 

Dark    shale 1,215  1,220 

Dark   shale  with  some   sandstone 1,220  1,225 

Dark    shale 1,225  1,235 

Dark   sandy  shale   and  laminated   sandstone 1,235  1,240 

Dark    shale 1,240  1,245 

Dark   sandy  shale   and   white,    fine-grained    sandstone,    apparently 

in   laminae.     Also  some   fragments  of  white  limestone 1,245  1,255 

Gray    shale,    greenish    fire    clay,    some    coal    and    a    little    nodular 

limestone     1,255  1,260 

Gray    shale    and    dark    shale,    some    yellow    siderite,    some    white 

limestone  and  a  few  fragments  of  coal.     Bituminous  joints....  1,260  1,270 
Gray    shale,    black    shale,    white    sandstone    of    fine    texture    and 

white    limestone 1,270  1,280 

Gray    shale,    considerable    white    limestone,    and    white    sandstone 

of  fine  compact  texture 1,280  1,285 

Black  shale  and  white  fine-grained  sandstone  with  some  limestone  1,285  1,290 
Fine-grained,  hard  white  sandstone,   gray,   sandv  shale  and  white 

limestone    1,290  1,295 

Micaceous  gray  sandstone,   black  shale,  and  some  pieces  of  white 

limestone    1,295  1,300 

Dark    gray   shale,    white    fine-grained    sandstone,    and    some    frag- 
ments   of    white    limestone 1.300  1,305 

Light   gray  micaceous  sandstone,   gray  shale  and  some  fragments 

of    white    limestone 1,305  1,310 

Dark  gray  shale,  laminated  sandstone  and  some  limestone 1,310  1,315 

White,    fine-grained    sandstone,    gray    shale,    white    limestone    and 

some   pyrite 1.315  1.320 

Sand,    fairly    coarse 1.320  1,325 

Yellow  rusty  sand 1,325  1,340 

Yellow  rusty  sand  with  some  shale 1,340  1.3  45 

Laminated  gray  sandstone   of  fine   texture 1.345  1.355 

Fine   sand,   with   some   shale   and   calcareous   material 1,355  1.360 

Fine  sand  and   shale,  with  some  carbonate  of  lime 1.360  1,365 

Fine   sand   and   shale 1,365  1,370 

Dark  gray   shale   and   sand 1,370  1,380 

Sand,  gray  shale  and  black  shale 1,380  1,405 

Greenish    gray    fire    clay,    some    dark    shale,    considerable    pyrite, 

and   sand    (from   above) 1,405  1,410 

Greenish    gray    fire    clay,    much    pyrite,    a    few    fragments    of   rock 

containing  organic  calcareous  fragments  and  some  sand 1,410  1,415 

Dark    greenish    gray    shale,    some    fragments    of    black    shale    and 

pyrite     1,415  1,420 


60 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.      [bull.  no.  22 


Logs — Continued. 


Depth  in  feet. 
From  To 


Sand  of  fine  texture  and  dark  greenish  gray  shale  or  fire  clay  with 

much    pyrite 1,420 

Dark  green   fire   clay   or   shale,   very  much   pyrite   and   fragments 

of   coal,   evidently   from  a   thin   seam 1,425 

Dark  greenish  gray  fire  clay,  pyrite  and  fragments  of  impure  coal  1,430 

Dark  green  fire  clay  and  dark  shale  with  some  coal 1,435 

Very  dark  shale,  thin  splitting  and  dark  green  fire  clay 1,440 

Very  dark  shale,  dark  green  fire  clay,  a  little  coal  and  pyrite 1,445 

Dark  green  fire  clay  and  dark  shale,  pyritiferous 1,470 

Dark  green  fire  clay-like  shale   1,480 

Dark  green  fire  clay-like  shale,  with  much  pyrite,  and  some  coal 

in  thin  seams 1,495 

Dark   green   fire   clay-like   shale    1,500 

Dark  green  fire  clay-like  shale,  some  black  bituminous  shale  with 

thin   laminae  of  coal,   and  with  pyrite 1,510 

Dark  green  fire  clay-like  shale,  dark  gray  shale,   "Coal  Measure"- 

like,    with    pyrites 1,515 

Dark  green  fire  clay-like  shale,  and  dark  gray  shale  with  pyrite.  .  1,520 
Brownish  red  marl,  some  fire  clay-like  greenish  shale,  some  pyrite 

and   some    fragments    of   white    limestone.      The    red    marl    and 

the  limestone  have  the  aspect  of  the  Chester 1,535 

Brownish  red  shale,  pyrite  and  fragments  of  white  limestone 1,540 

Red  marly  shale,  gray  marly  shale  and  white  limestone 1,545 

Dark  gray  shale   and  marl 1,565 

Dark   gray   stony   marl    and   fragments    of   white    limestone,    with 

crinoid    stems 1,570 

Gray  marl  and  red  marly  shale  with  fragments  of  white  limestone  1,590 
Gray,    green    and    red    shale,    white    limestone,    sandy    limestone, 

pyrite   and   crinoid   stems 1,595 

Greenish   gray   calcareous    shale 1,615 

Dark  green,    stony   calcareous   shale 1,635 

Dark    gray    shale,    organic,    fragmental    limestone,    dirty    specked 

gray    1,640 

Shale    and    limestone 1,645 

Gray  marly  shale  and  organic  fragmental  limestone     Oily 1,650 

Organic  fragmental  limestone  and  some  shale.     Oily 1,655 

Dark   gray  shale,   green  shale,   red  shale   and   organic   fragmental 

limestone.       Oily 1,660 

Like  the  preceding  with  less  limestone 1,665 

Red  marly  shale  and  green  laminated  shale 1,680 

Red  marly  shale  and  dark  green  shale 1,685 

Gray  marly  shale,  gray  sandstone  of  fine  texture  and  some  organic 

fragmental    limestone 1,695 

Gray   marly   shale 1,700 

Fine  gray  quartz  sand  showing  a  few  mica  scales  (and  effer- 
vescing)       1,730 

Fine-textured  gray  sand  with  some  shale 1,755 

Fine-textured  gray  sand  with  some  gray  shale 1,760 

Gray  marly  shale   and  sand 1,765 

Fine-textured  gray  sand,    dark   gray   shale,   with   some   fragments 

of  limestone  showing  joints  filled  with  black  bituminous  films..  1,775 

Gray   marly   shale   and   fine   sand 1,780 

Earthy  black  marly   shale  filled  with  bitumen 1,785 

Partly  like  the  preceding,  partly  gray  stony  marl 1,795 

Gray  marly  shale  and  fine  sand 1,800 

Like  the  preceding  with  some  very  thin-splitting  black  shale......  1,805 

Black  shale  and  fine  gray  sand 1,810 

Gray  marly  shale,  and  some  black  bituminous  material  shining  on 

conchoidally  fractured  surfaces     Fractures  and  fuses  in  flame..  1,820 

Gray    marly    shale 1,825 

Gray    marly    shale,    with    a    black    bitumen    showing    conchoidal, 

shiny    cleavage } .£  3  0 

Gray  marly  shale  with  a  few  small  fragments  of  bitumen 1,835 

Gray  marly   shale ;•"."'  L840 

Gray  marly  shale,   with   some  fine  micaceous   sand,   and  showing 

black    streaks J.»50 

Gray    marly    shale 1,860 

Almost  black  and  dark,  greenish  gray,  marly,  sandy  shale,  show- 
ing   red    streaks,    and    a    dark    greenish    sand    of    fine    texture. 

Mica    noted.      Oily ■ Vll\ 

Dark,   greenish  gray  fire  clay-like   shale.      Oily 1,880 

Dark   greenish-gray    shale    and    sandy   rock,    and    some    red    shale 

appearing   earthy,    from    bitumen •  1,885 

Green    and    red    shale,    with    some    fragments    of    sandstone    and 

some    organic    limestone.      Oily i  qia 

Oolitic   limestone,   and   green   shale I,yi0 

Oolitic  limestone,  other  limestone,  green  shale  and  some  red  shale. 

A  small  Dielasma  noted.     The  dark  green  shale  splits  into  very 

thin     fragments 1,915 


1,425 

1,430 
1,435 
1,440 
1,445 
1,470 
1,480 
1,495 

1,500 
1,510 

1,515 

1,520 
1,535 


1,540 
1,545 
1,565 
1,570 

1,590 
1,595 

1,615 
1,635 
1,640 

1,645 
1,650 
1,655 
1,660 

1,665 
1,680 
1,685 
1,695 

1,700 
1,730 

1,775 
1,760 
1,765 
1,775 

1,780 
1,785 
1,795 
1,800 
1,805 
1,810 
1,820 

1,825 
1,830 

1,835 
1,840 
1,850 

1,860 
1,865 


1,880 
1,885 

i,89a 

1,910 
1,915 


1,920 


BLATCHLEY] 


LAWRENCE    COUNTY    LOGS. 


61 


Logs — Continued. 


Depth  in  feet. 

From  To 

Green  shale,  dark  shale,  red  shale,  and  oolitic  limestone 1,920  1,930. 

Green    shale,    red    shale,    and    some    dirty    looking    limestone    and 

oolite.      Crinoid  stem  noted 1,930  1,945 

Mostly  iron  rust  from  bit  or  casing 1,945  1,950 

Limestone  with  a  great  deal   of  rust 1,950  1,955 

Granular  limestone  with  some  well-rounded  quartz  sand,  and  some 

oolitic  grains 1,955  1,960 

Granular    limestone,    gray 1,960  1,965 

Coarse  oolitic  limestone,   with  some  quartz   grains 1,965  1,970 

An  organic  breccia,  with  imbedded  oolitic  grains,  and  some  quartz 

grains 1,970  1,980 

Organic  fragmental   limestone,   with  oolitic  spherules,   and  with   a 

few   fragments    of   chert 1,980  1,995 

Limestone,    fragmental,    oolitic 1,995  2,000 

No.  3 

Operators — Snowden  Bros. 

Farm  and  well— H.  K.  Seed,  No.  3. 

Location — NW.  %  sec.  29,  Bridgeport  Township. 

Elevation— 513  feet. 


Soil,   yellow    

Slate,    dark    

Sand,  white   (12  bailers  of  water,   75  feet)    .... 

Slate,    dark    

Limestone,    white 

Slate,   dark 

Sand,    white    

Slate,    dark    

Limestone   shell    

Coal     

Slate,    dark    

Limestone,    light     

Slate,    light 

Sand,    light    

Limestone,    light    

Red  slate,   light    

Slate,   light    

Sand,  light,  hard    

Slate,    dark    

Sand,    light    

Slate,    dark    

Limestone,    dark 

Slate,   light    

Slate,    dark    • 

Sand,  light,  hard    

Slate,    light    

Coal     

Slate,    light    

Slight,    dark    

Limestone,    dark    .  .  .  . ; 

Slate,    dark    

Sand,  light   (hole  full  of  water,   905  feet)    

Limestone   and   sand,   light,    hard    

Slate,  black,  soft    

Slate,    light    

Limestone,    light    ". 

Slate     

Sand     

Slate     

Sand,    (hole  full  of  water,   1,140  feet)    

Slate,    dark     

Sandy  limestone,  light    

Slate,    black    

Limestone,    light    

Sand   and   coal    

Slate,    dark    

Sand    and    shells    

Slate,    dark    

Sand,   light,   hard    (water)    .'.'.' 

Slate,    dark,    soft    

Sandy  limestone,   light 

Sand,  light,  hard   (hole  full  of  water,  1,640  feet) 


Thickness 

Depth 

Feet 

Feet 

23 

23 

17 

40 

35 

75 

65 

140 

6 

146 

90 

236 

49  . 

277 

6 

283 

5 

288 

6 

294 

36 

330 

15 

345 

63 

408 

31 

439 

10 

449 

6 

455 

155 

610 

13 

623 

17 

640 

15 

655 

20 

675 

12 

687 

33 

725 

57 

782 

13 

795 

13 

808 

4 

812 

38 

850 

12 

862 

4 

866 

24 

890 

35 

925 

15 

940 

20 

960 

45 

1,005 

5 

1,010 

30 

1,040 

50 

1,090 

40 

1,130 

252 

1.382 

1,384 

41 

1,425 

2 

1,427 

23 

1,450 

17 

1,467 

2 

1,469 

1,470 

48 

1,518 

73 

1,591 

17 

1,608 

32 

1,640 

47 

1,687 

62 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.       [bull.  no.  22 


Logs — Continued. 


Thickness  Depth 

Feet  Feet 

Slate,    dark    16  1,703 

Sand,    dark    22  1,725 

Limestone,    light     4  1,729 

Red  rock 5  1,734 

Slate     31  1,765 

Limestone    21  1,786 

Slate     7  1,793 

Limestone     10  1,803 

Red   slate    7  1,810 

Sand    (water,    1,823    feet)     13  1,823 

Slate 10  1,833 

Limestone     20  1,853 

Slate     12  1,865 

Sand    (water,    1,872   feet)     7  1,872 

Red    slate     ■        6  1,878 

Slate     12  1,890 

Red   slate    4  1,894 

Sand    (water,   1,916   feet)    22  1,916 

Slate     6  1,922 

Sand   (hole  full  of  water,   1,947  feet)    25  1,947 

Slate     33  1,980 

Limestone     2  1,982 

Sand   (oil  pay,   1,982  to  1,995  feet)    19  2,001 

Total  depth    2,001 

NO.  k- 

Operators — Snowden  Bros. 

Farm  and  well — O'Donnell,  No.  28. 

Location — SE.  %  sec.  17,  Bridgeport  Township. 

Elevation — 498  feet. 


Thickness 
Feet 

Sand  and  mud    129 

Slate,    light    31 

Sand,  white    (10  bailers  water,   225  feet)    165 

Slate,    dark    10 

Limestone    shell,    hard    11 

Red   rock    9 

Slate,    light     120 

Slate,    dark    85 

Slate,    white    60 

Slate,    dark    100 

Slate,    black    15 

Sand,  white   (4  bailers  of  water,   750  feet)    45 

Slate,    light    , 25 

Sand,    light    10 

Slate,    dark    40 

Limestone   shell    6 

Slate,    dark    60 

Limestone    shell,    hard,    gray    4 

Slate,    dark    37 

Sand,  white,  hard   (oil,  970  feet ;  water,  990  feet) 86 

Slate,    light    2 

Sand,  white,  soft 20 

Slate,    light    25 

Sand,  white    40 

Slate,    dark    15 

Sand,    white    25 

Slate,    white    16 

Limestone,    light 12 

Slate,    dark    25 

Slate,    light     8 

Slate,    dark    44 

Sand,  dark   (oil,  1,298  feet) 38 

Sand,  light   (water,  1,360  feet)    77 

Limestone,    dark    15 

Slate,    dark    15 

Sand,    white    13 

Slate,    dark    9 

Limestone,    white     53 

Slate,    white    4 

Limestone    shell     2 

Slate,    dark 11 

Slate,    light    8 


Depth 

Feet 

129 

160 

325 

335 

346 

355 

475 

560 

620 

720 

735 

780 

805 

815 

855 

861 

921 

925 

962 

1,048 

1,050 

1,070 

1,095 

1,135 

1,150 

•    1,175 

1,191 

1,203 

1,228 

1,236 

1,280 

1,318 

1.395 

1,410 

1,425 

1,438 

1,447 

1,500 

1,504 

1,506 

1,517 

1,525 


Feet 

Feet 

35 

1,560 

25 

1,585 

8 

1,593 

32 

1,625 

13 

1,638 

12 

1,650 

26 

1,676 

54 

1,730 

12 

1,742 

15 

1,757 

8 

1,765 

3 

1,768 

10 

1,778 

12 

1,790 

8 

1,798 

15 

1,813 

22 

1,835 

20 

1,855 

20 

1,875 

15 

1,890 

333 

2,223 

2,223 

BLATCHLEY]  LAWRENCE    COUNTY    LOGS.  63 

Logs — Continued. 

Thickness     Depth 

Limestone,  white    

Slate,    dark    

Slate,   light    

Sand,  light   (show  of  oil,   1,600  to  1,606  feet)    

Slate,    dark 

Sand,    light    

Slate,    dark    

Sand,    light    

Slate,    dark     

Limestone,  light    

Sand   and.  limestone    

Red   slate 

Limestone,    light    

Slate,    dark     

Red   rock    

Slate,    light    

Limestone    ( ? ) ,   cavy    

Limestone     

Limestone,  gray,  hard,    (show  of  oil,  1,860  feet)    • 

Limestone,    gray,    soft    

Limestone,   dark,   hard    

Total  depth    

No.  5. 

Operators — Ohio  Oil  Company. 
Farm  and  well— W.  B.  Gray,  No.  2. 
Location — SW.  %  sec.  7,  Bridgeport  Township. 
Elevation— 486  feet. 

(This  record  was  compiled  by   Dr.   J.   A.  Udden  from  the  study  of  well 
samples.) 

Yellow  micaceous  sandstone,   with  some  quartz  pebbles 

White  micaceous  sandstone,  with  shreds  of  carbonaceous  matter.  . 

White  micaceous  sandstone,  with  some  fragments  of  siderite  and 
pyrite     

Gray  sandstone,  with  shreds  of  vegetation    

Gray   sandy   shale    

Black  shale  and  some  gray  micaceous  sandstone    

Black  micaceous   shale 

"Clod,"  with  numerous  crinoid  stems    

Black  shale  and  "clod"    

Coal    and    "clod" 

Coal,  fragments  of  siderite  concretions,  limestone  and  some  gray 
sandstone     

Gray   sandy   shale    

Black  shale,    "clod,"   some  coal   and   some  pure   calcite 

Dark  micaceous  shale  and  coal  with  calcite   

Dark  gray  micaceous  shale    

Black  shale,  with  a  few  crinoid  joints    

Black    shale     

Black  shale  with  some  limestone   

Black    shale     

Hard  black   shale    

Black   shale    

Black   micaceous   shale    

Gray  micaceous  sand,  with  some  black  shale    

Gray  micaceous  sandstone,  with  infiltrated  lime,  and  shreds  of 
carbonaceous    matter    

Gray  micaceous   sand    

Gray  sandstone,  some  black  shale,  and  a  little  limestone 

Black  shale  and  gray  sandstone,  with  a  little  limestone 

Dull  bluish  green  shale,  with  some  yellowish  limestone  from  con- 
cretions      

Like  the  preceding,  with  fossils  in  the  concretionary  limestone.  .  . 

Shale,  light,  green  gray  unctions,  shale 

Greenish   gray   micaceous    shale    

Light  greenish  gray  shale,   unctuous    

Light  greenish  gray  micaceous  shale'    

Gray   micaceous    sandy   shale    

Gray,  rather  coarse  sandstone  with  occasional  red,  pink,  green 
and    black    grains    

Like  the  preceding,  all  crushed 

Fire  clay,   fragments  of  concretions,   sandstone    


Depth  in 

feet. 

From 

To 

1 

10 

10 

30 

30 

35 

35 

40 

40 

45 

45 

50 

50 

55 

55 

60 

60 

65 

65 

70 

70 

75 

75 

80 

80 

90 

90 

95 

95 

100 

100 

105 

105 

110 

110 

115 

115 

120 

120 

130 

130 

135 

135 

140 

140 

145 

145 

155 

155 

205 

205 

210 

210 

215 

215 

220 

220 

225 

225 

240 

240 

245 

245 

250 

250 

265 

265 

270 

270 

275 

275 

280 

280 

285 

64 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.       [bull.  no.  22 


Logs — Continued. 


Depth  in  feet. 

From  To 

Fine  clay  and  some  shreds  of  carbonaceous  material   285  290 

Greenish  blue  shale,  with  concretionary  yellow  limestone    290  295 

Black  shale,  with  some  bits  of  coal    295  300 

Gray  micaceous  sandstone,  with  infiltrated  lime,  with   some  black 

shale  and   coal    300  305 

Gray  sandstone,  in  part  laminated,  with  small  siderite  concretions  305  310 

Gray  micaceous   sandstone  with   small   siderite   concretions 310  315 

Gray  sandstone  with  some  black  shale   315  320 

Dirty    white    limestone,    and    some    sand.      Pyrite,    crinoid    joints, 

and  spine  of  a  Productus  noted    320  325 

Limestone   and  some   shale    325  330 

Limestone  of  light  color,  some  gray  shale  and  pyrite.     Limestone 

seems  to  be   concretionary    330  335 

Gray  shale  and  black  shale  with  yellow  concretionary  limestone..  335  350 

Dark  gray  shale  and  some  yellow  concretionary  limestone   350  355 

Dark   gray  shale  with  some   pyrite    '355  360 

Dark  gray  shale,   some  white  limestone  and  pyrite    360  365 

Dark  gray  shale    365  380 

Dark   shale  with  some  fragments  of  siderite   concretions 380  390 

Sandstone,    shale   and   coal    390  395 

Shale,  with  some  sandstone  and  coal    395  400 

Greenish    gray    shale    400  405 

Olive  colored   shale    405  410 

Laminated  sandy  shale    '  410  415 

Sandy  gray   shale    415  420 

Shale,   stony,   olive   colored    420  425 

Gray   shale    425  430 

Dark   shale,   almost  black    430  435 

Gray   shale    435  460 

Gray  shale,  coal  and  concretion  fragments    460  465 

Gray  fire  clay,  coal  and  shale' 465  470 

Gray  shale,   and   gray  concretionary  limestone,    impure,   with   iron 

carbonate  and  with  pyrite    470  475 

Limestone,  concretionary  and  shale    475  480 

Gray    shaly    fire    clay    and    concretionary    limestone,    effervescing 

slowly     480  485 

Gray  concretionary  siderite    485  490 

Gray  shale,  with  much  concretionary  impure  limestone  or  siderite  490  515 

Gray  sandy  shale,  and  siderite    515  520 

Gray  micaceous  shale,  some  coal  and  siderite    520  535 

Gray  sandstone,  laminated  and  with  minute  spherules  of  siderite.  535  540 

Gray  shale,  with  some  sandy  shale  and  some  black  shale 540  545 

Dark   stony   shale    545  550 

Dark  micaceous  shale  with  some  limestone  with  crinoid  stem 550  555 

Dark  gray  shale    555  560 

Dark  micaceous  shale  and  clod  with  a  Productus 560  565 

Gray    shale    565  570 

Very  dark  shale  and  "clod" 570  575 

Black  clay  shale  with  "elod"    575  580 

Greenish  gray  micaceous  sandy  shale    580  590 

Gray  micaceous   shale    590  605 

Greenish   gray  clayey   shale    605  615 

Black  stonv  shale  and  some  red  clay  shale    615  620 

Very  dark  stony  shale    620  625 

Dark  cheeky  shale  or  fire  clay   625  630 

Dark   gray  micaceous  shale    630  635 

Dark  shale  or  fire  clay,  with  imprint  of  leaf 635  640 

Dark  hard  shale,  slightly  micaceous    640  645 

Gray  shale,  with  some  siderite    645  650 

Gray   shale    650  655 

Gray  shale  and  some  gray  sandstone    655  660 

Hard  gray  shale,  with  a  few  pieces  of  sandstone    660  665 

Hard  gray  shale,  with  a  few  pieces  of  siderite   665  670 

Dark  and  hard  shale    670  675 

Dark   hard   shale    675  685 

Coal  and  dark  shale,  with  some  siderite  and  pyrite    685  690 

Coal,  with  some  shale  and  some  siderite    690  695 

Dark  shale  and  some  siderite,  coal,  and  pyrite,  bit  of  sh^U  noted.  .  695  700 
Gray  shale  and  coal,  with  concretions  of  siderite,  and  black  shale, 

with   leaf   imprints,    calcareous    700  705 

Gray  shale,   fire  clay  and   coal,   calcareous    705  710 

Gray  shale  and  fire  clay  calcareous    710  715 

Like  the   preceding,   with  wood   in   pyrite    715  720 

Gray   clay   shale,    fine   in    texture    720  725 

Black   shale,    sandstone,   and  coal    725  730 

Gray  sandstone  and  dark  gray  sandy  shale    730  740 

Gray  sandstone,  and  shale    740  755 

Black    miner's    slate 755  760 

Dark   shale,    carrying  much   fine   pyrite    760  765 


From 

To 

765 

770 

770 

775 

775 
780 

780 

785 

785 
790 
795 
800 

790 
795 
800 
805 

805 

810 

810 
815 
830 

815 
830 
835 

835 

840 

840 
845 
850 

845 
850 
855 

855 
860 
865 

860 

865 
875 

875 
880 

880 
890 

890 
895 

895 
900 

BLATCHLEY]  LAWRENCE    COUNTY    LOGS.  65 

Logs — Continued. 

Depth  in  feet. 

Gray  shale,   impregnated  with   small   pyrite   crystals 

Gray  shaly  sandstone  and  black  shale    

Coal,  sandstone  and  some  yellow  limestone  (apparently  from 
a  ledge )    

Gray  micaceous  and  sandy  shale,  some  red  clay  shale 

Gray  shale,  coaly  shale  and  shaly  coal,  with  gray  limestone  and 
fragments   of   concretionary   siderite    .  .  . 

Gray  clay  shale,  with  some  concretionary  fragments   

Gray  shale,  some  black  shale  and  siderite  concretions 

Gray  shale,  some  black  carbonaceous  shale  and  some  fire  clay .  .  . 

Gray  shale,  some  black  coaly  shale,  a  few  bits  of  white  limestone 
and  minute   concretionary   spherules    

Gray  shale  containing  many  minute  spherules  of  siderite  and 
some  white  limestone   

Dark  shale  and  fire  clay 

Dark  shale,  with  some  imprints  of  vegetation    

Dark  shale  and  some  sandstone,  with  some  minute  spherules  of 
siderite     

Black  shale  and  gray  shale,  with  some  sandstone,  some  minute 
spherules  of  siderite  and  a  few  bits  of  limestone   

Black  shale,  some  sandstone  and  some  pieces  of  siderite 

Gray  micaceous  shale    

Black  hard  shale,  with  pyrite,  shell  of  Retzia  (?),  some  spicules 
and  a  few  bits  of  white  limestone   

Black  stony  shale,  with  pyrite    

Black  shale,  with  pyrite  and  pieces  of  siderite   

Black  shale,  and  white  fine  grained  sandstone,  laminated  with  a 
few  small  pieces  of  very  white  limestone   

Gray  laminated  sandstone  and   black   shale    

Black  shale  and  laminated  sandstone,  with  some  grayish  soft 
material  and  a  few  bits  of  white  limestone   

Coal,  with  some  gray  limestone    

Gray   sandy   shale   and   fragments   of   concretionary   siderite,    with 

some    coal    900  905 

Black  shale  and  gray  shale,  with  some  fragments  of  yellow  lime- 
stone and  concretionary  material    905  910 

Dark  gray  shale,  with  a  little  limestone,  and  some  green  serpen- 
tine-like   shale    910  915 

Dark  gray  shale  and  greenish  shale  with  red  blotches,  with  a  few 
fragments   of  limestone    

Dark  gray  shale   and   gray  sandy   shale 

Gray  sandy  shale  with  minute  crystals  of  pyrite    

Dark  gray  shale  and  gray  sandstone,  with  shreds  of  vegetation .  . . 

Dark  gray  shale  and  some  sandstone 

Gray  shaly  sandstone  and  sandy  shale   

Dark   gray  sandy   shale,    pyritiferous    

Dark  gray  sandy  shale    

Gray  clay   shale    , 

Gray  shale  and  limestone.  The  limestone  is  white,  and  consists 
of  rounded  fragments  which  are  invested  with  an  oolitic  incrus- 
tation      

Dark  and  stony  thin  splitting  shale  and  light  sandstone 

White  and  gray  sandstone  and  dark  gray  shale.  Sandstone  occa- 
sionally with   interstitial   pyrite    

Dark  gray  shale  and  white   sandstone    

Dark  greenish  gray  shale    

Black   shale   of  fine   texture    

Dark  gray  shale,  with  siderite  partly  in  fragments,  partlv  as 
spherules    

Dark   gray  sandstone   and   dark   shale    

Dark  shaly  sandstone  and  black  shale    

Black  shale,  with  many  fragments  of  siderite    

Black    shale    

Black  shale,  and  gray  limestone  which  contains  a  tangle  of 
tubes  of  Ammodiscus    

Dark  gray  and  black   shale  with  limestone  as   above ......'...'..'. 

White   and  gray  sandstone   and   gray  shale    

White,   slightly  micaceous   sandstone   and   gray   shale 

Gray  laminated  shaly  sandstone    

Gray    sandstone     

Laminated  gray  sandstone  and  white  sandstone 

Yellow    sandstone    

Coarse  white   sand    ' 

Yellow    sand 

Red    sand 

White   sand,    finer 

Reddish   sand '.        ..'... » 

Gray    sand \  ..'.'.'.'.'.'.'.'.'.'.'.'.I'.'.'.'.'.'.  .'.'.'.'.'.'.'.'.'.'.'.'.'.I 

—5  G 


915 

920 

920 

925 

925 

930 

930 

935 

935 

940 

940 

945 

945 

950 

950 

955 

955 

960 

960 

965 

965 

970 

970 

975 

975 

985 

985 

1,000 

1,000 

1,005 

1,005 

1,010 

1,010 

1,015 

1,015 

1,020 

1,020 

1,025 

1,025 

1,030 

1.030 

1,035 

1,035 

1,040 

1,040 

1,045 

1,045 

1,050 

1,050 

1,060 

1,060 

1.080 

1,080 

1,100 

1,100 

1,105 

1,105 

1,115 

1,115 

1,125 

1,125 

1,135 

1,135 

1,165 

1,165 

1,175 

1,175 

1,185 

'66 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


Logs — Continued. 


Depth  in  feet. 


To 

1,195 
1,200 
1,205 
1,210 
1,215 

1,220 

1,230 
1,240 
1,245 
1,250 


1,345 
1,350 


1,370 


1,373" 
1,385 
1,390 
1,395 
1,435 


From 

White    sand 1,185 

Black  shale,  with  some  few  small  fragments  of  red  shale   (?)'.'.!.!         1,195 

Black  shale  and  sand  with  pyrite 1,200 

Gray  fire  clay  with  shreds   of  vegetation L205 

Black  clay  shale,  gray  sand 1,210 

Black  shale,   gray  fire   clay-like   shale  with   shreds   of  vegetation 

and   sandstone 1,215 

Dark  fire   clay,   shale,   with  shreds  of  vegetation   with  some   gray 

sand    1,220 

Fire  clay,  dark  shale  and  sandstone 1,230 

Gray   shale    and    sand 1,240 

Gray  fire  clay,  and  gray  sandstone  with  spherules  of  siderite 1,245 

Black  stony  shale  with  large  fragments  of  pyrite  and  some  gray 

compact   siliceous    rock 1,250         1,260 

Black  shale  showing  shreds  of  vegetation  and  some  gray  rock 1,260         1,280 

Laminated   dark   and   gray   sandy  and   stony    shale   showing   mica 

and  shreds  of  vegetation,  very  much  comminuted 1,280 

Black  shale  with  pyrites  and  some  sandstone 1,345 

Coarse  sand  showing  secondary  enlargement  of  grains,  with  some 

black    shale 1,350 

Diameter  Percentage 

of  grains  of  total 

in  mm.  sample. 

2-1 0 

1-%       5 

1/2-1/i       10 

%-%     80 

Less  than  y8  5.00 

Gray  sand  of  somewhat  finer  texture  than  the  preceding 1,370 

Gray  coarse  sandstone  and  some  black  shale 1,375 

Like  the  preceding,  but  with  finer  sand 1,385 

Coarse   sand  and  some  gray  shale 1,390 

Sand,   white 1,395 

Diameter  Percentage 

of  grains  of  total 

in  mm.  sample. 

2-1        0 

1-%       3 

%-%     6 

%-%     85 

Less  than  y$         6 

White    sand 1,435 

Fine   reddish   sand 1,455 

Fine   gray   sand 1,460 

Fine    yellow    sand 1,465 

White  limestone,  with  some  sand 1,480 

Like  the  preceding,  with  two  minute  echinoid  stems 1,485 

Yellowish    organic    limestone 1,490 

White   limestone   containing  fragments   of  fossils   and  with   a   few 

fragments  of  chalcedonic  chert  and  with  much  dark  shale 1,495 

Organic   calcareous   fragments   with   dark   shale   and   coarse   white 

sand     1,500 

Dolomitic    ( ?)    limestone,    with    an    occasional    purple    tint,    mixed 

with  much   shale  and   sand 1,515 

Yellowish  sandstone,  with  some  shale  and  dolomitic  (?)  calcareous 

fragments    1,520 

Limestone,  organic,   fragmental  gray,  calcareous,  with  some  shale 

and  sand.      Some  shale   is   green 1,530 

Dark  gray  organic  fragmental  limestone,  with  some  green  shale.  .         1,545 

Like  the  preceding,  with  more  shale 1,550 

Gray  and   greenish   shale   and   gray   calcareous   limestone,   with   a 

fragment    of    a    fossil    shell 1,555 

Gray   calcareous   organic   limestone    and   greenish   shale 1,560 

Fine  gray  sand  and  shale  with   pyrite 1,565 

Gray  sandstone   and  shale 1,570 

Dark  gray  shale,  gray  sandstone  and  limestone 1,575 

Black  shale,  showing  a  few  brown  blotches 1,580 

Black  shale,  with  green  and  red  shale,  some  limestone  and  pyrite..  1,585 
Dark  gray  shale,  with  green  and  some  red  shale  and  limestone....  1,590 
Like  the   preceding,   with  two  thin   flakes  of  coal  and   a   few  bits 

of    red    limestone 1,600 

Dark   gray   and   greenish   gray   shale,    some   white   sandstone    and 

some  red  shale,  with  some  fragments  of  limestone 1,605 

Like   the   preceding  but  more   sandy.      Pyrite 1,610 

Gray  fine  sand,  gray  and  black  shale  and  limestone  and  pyrite 1,615 

Gray  fine  sand  and  dark  gray  shale 1,620 

Black  and  greenish  shale  with  sandstone  and  pyrite 1,625 

Black    shale,    and    gray    sand 1,630 


1,455 
1,460 
1,465 
1,480 
1,485 
1,490 
1,495 

1,500 

1,515 

1,520 

1,530 

1,545 
1,550 

1,555 

1,560 
1,565 
1,570 
1,575 
1,580 
1,585 
1,590 
1,600 

1,605 

1,610 
1,615 
1,620 
1,625 
1,630 
1,635 


Depth 

in  feet. 

From 

To 

1,635 

1,640 

1,640 

1,645 

1,645 

1,650 

1,650 

1,655 

1,655 

1,660 

1,660 

1,665 

1,665 

1,670 

1,670 

1,675 

1,675 

1,685 

1,685 

1,695 

1,695 

1,700 

1,700 

1,710 

1,710 

1,715 

1,715 

1,740 

1,740 

1,750 

1,750 

1,760 

1,760 

1,765 

1,765 

1,775 

1,775 

1,780 

blatchley]  LAWRENCE   COUNTY   LOGS.  67 

Logs — Continued. 


Black  shale  and  gray  sandy  shale,  with  bits  of  red  shale 

Gray    shale 

Black  shale,  greenish  shale  and  sandstone 

Greenish  gray  shale  and  some  white  sand 

Gray  and  green  shale  with  sand.     One  fragment  of  bitumen  noted, 

which   burned    when    ignited 

Black  and  gray  shale  and  sand  in  about  equal  quantities 

Slickensided  greenish  gray  shale  and  fine  sand 

Sandstone   and   dark   shale 

Sandstone,   dark  shale  and  some  calcareous  lime 

Gray   fine   sand 

Sand  and  dark  shale 

White  limestone,  dark  gray  shale  and  sand  effervescing  slowly. . . . 

Fine    yellow    sand 

Fine    gray   sand 

Black  and  dark  gray  shale 

Dark  gray  shale  and  some  gray  limestone,  oolitic  grains   (?) 

Grayish  white   fine   sand 

Grayish  white  sand  and  some  shale,  effervescing  slowly 

Dark  gray  and  black  shale  with  some  sand 

Calcareous  limestone  with  slow  effervescence   and   dark  gray  and 

red  shale  oolitic  grains   1/2-1A   mm.  in  diameter 1,780        1,785 

Gray  calcareous  limestone   with  bits   of  brachiopod  shells,   spines, 

occasional    oolitic    grains,    and    dark    gray    and    dull    red    shale. 

Oolites   frequently   oval 1,785         1,795 

Like  the  preceding,  with  more  sand  and  more  oolitic  grains 1,795        1,800 

Dark   shale,    some    oolitic   limestone 1,800         1,805 

Dark  shale,  oolitic  limestone  and  some  red  shale 1,805        1,810 

Dark    shale,     red    shale,     oolitic    limestone    and    lobster    colored 

limestone     1,810         1,815 

Like  the  preceding  but  with  less  limestone 1,815         1,825 

Dark    greenish    gray   shale,    and    dark    red    shale   with    limestone, 

organic    1,825         1,830 

Like  the  preceding,  with  a  few  limestone  fragments   of  "lobster" 

red    color 1,830         1,835 

Dark  gray,  gray  and  red  shale  with  organic  limestone,  with  slow 

effervescence    

Oolitic  limestone  effervescing  slowly  and  black  and  red  shale 

Ooolitic  white   calcareous   limestone 

Gray  limestone   effervescing   slowly 

Fiwe  gray  sand,  pure,  grain,  measuring  about  1-6  mm.  in  diameter 

Gray  limestone,   effervescing  slowly  with  acid 

Gray   limestone,    calcareous 

Gray  calcareous  limestone  with  a  few  bits  of  chalcedonic  chert 

Gray  limestone,  with  slow  effervescence,  with  some  fragments  of 

chert     

Gray  oolitic  calcareous  limestone 

Gray    oolitic    limestone    effervescing    slowly,    fragments    of    ribbed 

lamellibranch    noted 

Gray  oolitic  limestone,   effervescing  slowly 

Gray    marl 

Gray  marl  ji.nd  some  limestone 

Gray   very   finely   granular   dolomitic    and    oolitic    limestone,    with 

chalcedonic    chert 1,985         2,000 

No.  g. 

Operators — Bridgeport  Oil  Company. 
Farm  and  well — McPherson,  No.  3. 
Location — SE.  %  sec.  11,  Lawrence  Township. 
Elevation— 429  feet. 

Thickness  Depth 

Feet  Feet 

Limestone     9  90 

Slate     65  155 

Sandy    limestone    45  200 

Slate     15  215 

Coal     5  220 

Slate     15  235 

Limestone     15  250 

Slate     150  400 

Limestone     40  440 

Slate     100  540 

Limestone     8  548 

Slate     52  600 


1,835 

1,855 

1,855 

1,865 

1,865 

1,890 

1,890 

1,895 

1,895 

1,900 

1,900 

1,905 

1,905 

1,948 

1,940 

1,945 

1,945 

1,950 

1,950 

1,965 

1,965 

1,970 

1,970 

1,975 

1,975 

1,980 

1,980 

1,985 

68 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


Logs — Continued. 


Limestone     

Sand,    (hole  full  of  water,  625  feet)    

Slate     

Sand    

Slate    

Limestone     

Slate     

Sand    

Slate 

Sandy    limestone    ' 

Sand    (water)     

Slate    

Limestone     

Sand    

Limestone     

Red   rock    

Slate     

Limestone     

Slate     

Limestone     

Red  rock    

Slate    

Limestone     

Slate    

Red  rock    

Slate    

Sand   (first  oil,  1,520  feet;  best  oil,  1,543  feet) 

Limestone     

Slate     

Sand     

Limestone     

Slate    

Limestone     

Sand  (water,  1,766  feet)    

Total  depth   


Thickness 

Feet 

5 

95 

45 

30 

115 

6 

44 

50 

5 

35 

30 

Depth 

Feet 

605 

700 

745 

775 

890 

896 

940 

990 

995 

1,030 

1,060 

165 

1,225 

1,280 

52 

1,332 

10 

1,342 
1,365 

23 

1,372 

3 

1,375 

1,410 

20 

1,430 

1,440 

20 

1,460 
1,480 

10 

1,490 
1,505 
1,518 
1,567 
1,590 

13 

23 

1,645 
1,660 
1,670 

15 

15 

1,685 

1,762 

6 

1,768 

1,768 


No.  7. 


Operators — Bridgeport  Oil  Company. 
Farm  and  well — McPherson,  No.  4. 
Location- 
Elevation — 425  feet. 


Thickness  Depth 

Feet  Feet 

Gravel   and   quicksand    85  85 

Sand     25  110 

Slate     28  138 

Limestone     7  145 

Slate    55  200 

Sand     , .  30  230 

Limestone     5  235 

Red    rock    5  240 

Limestone     10  250 

Slate     140  390 

Limestone     5  395 

Coal     5  400 

Limestone     40  440 

Slate    90  530 

Limestone     10  540 

Slate    45  585 

Sand    (water)     90  675 

Slate     15  690 

Sand     35  725 

Slate     65  790 

Sand    15  805 

Slate     65  870 

Sand    10  880 

Slate    20  900 

Limestone     5  905 

Slate    50  955 

Sand    (water) 45  1,000 

Slate    : 2  1,002 

Sand    63  1,065 

Limestone    10  1,075 


BLATCHLEY] 


LAWRENCE   COUNTY   LOGS. 


69 


Logs — Continued. 


Thickness  Depth 

Feet  Feet 

Slate     105  1,180 

Sand     8  1,188 

Limestone     2  1,190 

Slate 140  1,330 

Sand    20  1,350 

Limestone     5  1,355 

Slate    15  1,370 

Limestone     89  1,459 

Red    rock     8  1,467 

Limestone     8  1,475 

Slate 34  1,509 

Limestone     13  1,522 

Slate    • 5  1,527 

Sand    (show  of  oil)     19  1,546 

Slate     12  1,558 

Sand   (oil  pay,   1,558%.  feet;  water,   1,563   feet)    17  1,575 

Slate    25  1,600 

Limestone    50  1,650 

Slate     15  1,665 

Limestone 5  1,670 

Slate     15  1,685 

Red   rock    10  1,695 

Slate     5  1,700 

Limestone     71  1,771 

Sand 4  1,775 

Limestone     83  1,858 

Sandy    limestone     6  1,864 

Limestone     122  1,986 

Total    depth    1,986 

No.  8. 

Operators — Bridgeport  Oil  Company. 
Farm  and  well — R.  M.  Kirkwood,  No.  7. 
Location — NE.  *4  sec.  14,  Lawrence  Township. 
Elevation— 435  feet. 


Thickness 
Feet 

Sand  and  gravel 83 

Limestone    10 

Slate     32 

Limestone     15 

Slate    70 

Sand    (water)     25 

Slate     10 

Limestone     5 

Slate 45 

Limestone     5 

Slate     25 

Limestone     20 

Slate     95 

Sand    10 

Slate     180 

Sand    (water)     87 

Slate     38 

Limestone    8 

Slate    10 

Sand    27 

Limestone     20 

Slate     40 

Sand     20 

Slate     20 

Sand     20 

Slate     40 

Sand    (water)     90 

Slate     : 120 

Sand     10 

Slate    50 

Limestone     6 

Slate    8 

Limestone    21 

Slate     11 

Limestone     9 

Sand     85 


Depth 
Feet 
83 
93 
125 
140 
210 
235 
245 
250 
295 
300 
325 
345 
440 
450 
630 
717 
755 
763 
773 
800 
820 
860 
880 
900 
920 
960 
,050 
.170 
,180 
,230 
,236 
,244 
,265 
.,276 
1,285 
1,370 


70 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,      [bull.  no.  22 


Logs — Continued. 

Thickness 
Feet 

Slate    30 

Limestone     20 

Slate    15 

Limestone     30 

Slate     3  0 

Limestone     25 

Red   rock    15 

Slate 5 

Sand    (oil,   1,551   feet)    40 

Slate    5 

Sand    (water)     5 

Slate    5 

Sand    10 

Slate    5 

Limestone     20 

Slate    20 

Sandy   limestone    25 

Slate    20 

Limestone 10 

Red    Rock 5 

Limestone     57 

Sand    8 

Total   depth    


Depth 
Feet 

1,400- 
1,420 
1,435 
1,465 
1,495 
1,520 
1,535 
1,540 
1,580 
1,585 
1,590 
1,595 
1,605 
1,610 
1,630 
1,650 
1,675 
1,695 
1,705 
1,710 
1,767 
1,775 

1,775 


No.  9. 

Operators — Snowden  Bros. 
Farm  and  well — Cummings,  No.  12. 
Location — NE.  %  sec.  6,  Bridgeport  Township. 
Elevation— 516  feet. 


Thickness  Depth 

Feet  Feet 

Soil     25  25 

Slate     102  127 

Limestone,   gray,   soft 8  135 

Sand,    white 45  180 

Slate,   dark 12  192 

Sand,    light 80  272 

Slate,    dark 20  292 

Limestone,   light,   hard 13  305 

Slate,    light,    soft 18  323 

Slate,   dark 257  580 

Limestone,    light 9  589 

Slate,     dark 311  800 

Limestone,    light,    hard 4  804 

Slate  and  limestone   shells,   dark,    soft 126  930 

Sand,   light   (little  oil,   940  feet) 40  970 

Slate   and   limestone   shells 15  985 

Sand,    light 15  1,000 

Slate,   light    (water,    1,006    feet) 20  1,020 

Slate   and   limestone    shells 45  1,065 

Slate,    white 70  1,135 

Sand,   light,   soft 15  1,150 

Slate,     black 15  1,165 

Sand,  white   (water,  1,175  feet) 50  1,215 

Slate,    white ' 5  1,220 

Limestone,    white,    soft 20  1,240 

Slate,  white,   hard 30  1,270 

Sand     5  1,275 

Slate,    light,    soft 5  1,280 

Limestone,    white 14  1,294 

Slate,    dark 21  1,315 

Limestone,    gray 16  1,331 

Slate,    dark 14  1,345 

Sand,   gray    (gas,   1,347   feet) 18  1,363 

Slate,    light 3  1,366 

Limestone,     white 19  1,385 

Slate,    dark 4  1,389 

Sand,    gray 7  1,396 

Slate,    light 19  1,415 

Red   slate 10  1,425 

Sand,    light    (oil,    1,428    feet) 15  1,440 

Slate,    light 15  1,455 


BLATCHLET] 


LAWRENCE    COUNTY    LOGS. 


n 


Logs — Continued. 


Thickness 
Feet 

15 

Sand,    light 7 

Red   slate •  •  •  •  •  •  •  •  •  • 33 

Slate  and  limestone  shells,  dark 15 

Limestone,    light 35 

Slate,    white 5 

Sand   and   limestone   shells,   white ? 

Slate,     white 28 

Limestone,    white ....  ^ 

Slate,     white 3  ± 

Limestone,    light.. ■•„•••  •••;• 3 

Sand   (show  of  oil  and  gas,   1,656   feet) ■  •    ■  lg 

Limestone     '  '  3 

Sand .'.".'.'.*.'!."!  58 

Limestone     • 

Total    depth 


Depth 
Feet 
1,470 
1,477 
1,510 
1,525 
1,560* 
1,565 
1,572 
1,600 
1,625 
1,656 
1,659 
1,672 
1,675 
1,733 

1,733 


NO.  10. 


Operators— Ohio  Oil  Company. 

Farm  and  well— S.  G.  McCleave,  No.  4. 

Location— Center  of  section  31,  Bridgeport  Township. 

Elevation — 520  feet. 

Thickness 
Feet 

1 

YeHow'  "limestone '  and"  "coai," '  some  '  pieces' '  of '  pure    calcite,    and  ^ 

CoaryeTlow  santtont^me  crinoidal"  limestone"  and"  "a  "few"  "pieces 

of'  calcite  and  red  marl.     Numerous   crinoid  stems. ^ 

Coal,  yellow  sandstone,  some  crinoidal  limestone  and  a  few  pieces 

of  calcite  and  red  marl.     Numerous  crinoid  stems •  •  &* 

Gray  micaceous  sandstone  with  infiltrated  lime,  some  yellow  sand- 
stone    bits   of   coal   and   calcite , •  •  •  •.•  •  •.  ■  •  • 

Coal    some  yellow  and  white   sandstone,   some  pieces  of  crinoidal  ^ 

Gray  nifcaceous'  sandstone",'  some  dark"  shale  and  fire  clay   ...  .  . . . 

CoaL     Some  crinoidal  limestone,  a  little  red  oxidized  material.     A 

small  Athyris  shell  noted,  also  a  piece  of  crinoid  calyx   (?) . ...  45 

White  micaceous  sandstone,  a  few  pieces  of  fire  clay  and  coal   ...  50 

Gray   micaceous   laminated   sandstone,    some   fragments   of   yellow  ^ 

Gr^S^  70 

Yenow  sandstone,'  crinoidal'  "limestone, 'some  black  shale  and  pieces 

of  gypsum.     Two  Ambocoelia  planoconvexa  and  a  crinoid  stem  ^ 

Bla?kdshale,"  'some  dark  "limestone,"  'and*  a  few'  pieces  'of  'sandstone.  ^ 
A    crinoid    stem    noted •  • •  •  ■  •  ■  •  • op- 
Gray  limestone  and  coal,  with  some  sandstone  and  shale 85 

YenowmnmeCsToUne  "som'e  'gray  "sandstone",  "and  bits  "of  'siderite ." ." ." ' !  I '  95 

Yellow  ttstone    and   #-ay    sandstone,    some    siderite    concretions  ^ 

and   shale 10  5 

§Sk  Ihalt^omf  sM^Se "concretions,  "and "bits"  of  "wh^  '^^ne  110 

Coll.    some    black    shale,    gray    sandstone,    a    few    bits    of    cakute  ^ 

GW   micaclou's'  'sandy' '  shale," '  some  '  dark  '  shale* '  and  '  coal,    some 

pieces  of  yellow  limestone  and  fire  clay. |£" 

Dark  shale    some  coal,  a  few  pieces  of  limestone. j£j> 

Bark  sha  e,'  soSI  red  oxidized  material,  and  siderite  concretions.  .  130 

Coal,  some  gray  micaceous  shale,  and  gray  sandstone 135 

Grav  micaceous  shale,   some  coal   and  fire  clay..... +v"' 

Gray   micaceous    shale    and   sandstone,    some    siderite    concretions, 

a   few   bits   of   white    limestone •  • -. •• t:Kn 

Gray  micaceous  shale  and  a  few  bits  of  siderite  concretions 150 

Siderite,   concretionary,  some  gray  micaceous  shale ^ . .  .  . . . .  •  • 

Coal  and  gray  sandstone,  some  concretionary  siderite,  some  bits  of 

limestone  and  pyrite.     A  crinoid  stem  noted jou 

White  sandstone  with  infiltrated  lime ^80 

Fine  gray  sand  with  infiltrated  lime :•••,■. "  * ' ' ' ' "  " 

Fine     gray    micaceous     sand     with     infiltrated     lime,     some     gray  ^ 

shale    "■  ■ : '  ion 

Fine  gray   sand  with  infiltrated  lime 


Depth 

Feet 

15 

20 

25 

30 

35 

40 
45 

50 
65 

70 

75 

80 

85 
90 
95 

100 

105 
110 
115 

120 

125 

130 
135 
140 
145 

150 
155 
160 

165 
180 
185 

190 
210 


72  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 

Logs — Continued. 

Thickness     Depth 
Feet  Feet 

White   micaceous   sand 210  225 

Sand,  with  infiltrated  lime,   and  some   coal 225  230 

Coal,   some  white   limestone  and  black  shale,   some  siderite 230  235 

Gray   micaceous   shaly   sandstone,    some   bits    of   coal,    pyrite,    and 

siderite    235  240 

Yellow    sand    with    infiltrated    lime ;    the    smaller    grains    float    on 

water    240  245 

Gray  micaceous  sandstone,  some  small  spherules  of  siderite  con- 
cretions,  a  few  pieces  of  pyrite  and  white  limestone 245  250 

Gray  sandstone,  some  siderite  concretions    (spherules),  some  dark 

shale,    and   bits   of   white    limestone 250  255 

Dark  sandy  micaceous  shale,  some  gray  sandstone,  and  siderite..  255  265 

White    sandstone 265  280 

Gray  micaceous  sandstone,   some  pieces  of   laminated  sandstone..  280  310 

White   micaceous   sand 310  320 

White   limestone,   indistinctly   fragmental,    a   little   sand   and   some 

gray    shale 320  325 

White    limestone    like   the   above,    a   little    dark   shale.      A    crinoid 

stem    noted 325  330 

White,  indistinctly  fragmental  limestone.     Some  bits  of  pyrite,  and 

a  crinoid   stem   noted 330  335 

Greenish  compact  limestone,  and  micaceous  sandstone,   with  some 

shale     335  340 

Gray  shale,   some   sandstone 340  345 

Gray   micaceous   sandy   shale 345  350 

Gray  micaceous  shale,  some  yellow  limestone,  and  one  piece  con- 
taining woody  fibre    (?) 350  355 

Gray    sandy    shale,    some    yellow    limestone,    and    a    few    siderite 

concretions     355  360 

Gray  shale,  micaceous  sandy  shale,  and  some  yellow  limestone....  360  365 

Gray   sandstone,    some    laminated   yellow    sandstone,    some    yellow 

limestone,    fragments    of    siderite 365  370 

Gray  shale  and  sandstone,    some   siderite   concretions 370  375 

Gray  sandy  shale,  some  siderite  concretions.     Carbonaceous  shreds 

noted    in    shale 375  380 

Siderite   concretions,    some    sandy    shale 380  385 

Gray   sandy   shale,    some   concretionary   siderite    and    bits   of   gray 

sandstone     385  390 

Gray  sandstone  and  sandy  shale.  A  few  pieces  of  black  car- 
bonaceous shale,  coal,  some  sandstone  with  infiltrated  lime, 
and  some  crinoid  stems.     Retzia  punctulifera  noted   390  395 

Gray  sandstone,  dark  shale,  some  white  limestone,  concretionary 
siderite.  A  crinoid  stem  and  Athyris  noted.  A  little  coal 
noted     395  400 

Gray    shale    and    some    sandstone,    concretionary    siderite,    bits    of 

pyrite,  and  a  few  pieces  of  sandstone  with  infiltrated  lime 400  405 

Gray  sandy  shale,   and  some  concretionary  siderite    405  410 

White  brexiated  limestone,  with  cracks  filled  with  yellow  calcite, 
some  yellow  limestone,  some  siderite,  a  little  gray  shale,  and 
sandstone  with  bits  of  pyrite    410  415 

White  limestone,  cracks  filled  with  yellow  calcite,  some  concre- 
tionary   siderite    415  420 

White    limestone,    having   cracks    filled    with    yellow    calcite,    some 

yellow  limestone,   some  gray  soft  shale,   and  a  few  bits  of  coal  420  430 

White  and  yellow  limestone,   cracks  filled  with  calcite,   some  gray 

sandstone  and  a  few  pieces  of  black  shale    430  435 

Gray  shale  and  concretionary  siderite 435  450 

Dark   gray  shale  and   siderite   concretions    450  475 

Gray  sandy  shale,  some  gray  sandstone,  siderite,  and  a  few  frag- 
ments of  yellow  limestone    475  480 

Gray   sandy  shale,    some  pieces  of  which   have   layers  of  siderite, 

yellow  limestone  and  bits  of  pyrite    480  485 

Gray  micaceous  shale,  some  gray  sandstone,   few  small  fragments 

of    yellow   limestone    485  490 

Gray  micaceous   shale    490  495 

Dark  shale,  some  siderite  concretions,  a  few  pieces  of  white  lime- 
stone   and    pyrite 495  500 

Dark  shale,  some  coal  and  concretionary  siderite,  and  a  few 
pieces  of  dark  limestone.  A  crinoid  stem  noted,  also  some 
oolitic    black    concretionary    material    500  505 

Dark  shale  and  some  siderite,  a  few  bits  of  white  limestone,  coal, 
and  pyrite.  Crinoid  stem  and  closely  tuberculated  crinoid  spine 
moted,  also  a  spiral  Ammodiscus.  Rhombopora,  lepidoden- 
<droides,  and  black  shale  with  fucoidal  traversions    505  510 

Dark  shale,  some  siderite,  white  limestone,  fragments  and  bits 
of  coal  and  pyrite.  Crinoid  stems  and  a  small  Syntrielasma 
hemiplicate    noted    510  515 

Gray  micaceous  shale,  some  gray  sandstone  and  yellow  limestone  515  520 


blatchley]                                 LAWRENCE   COUNTY   LOGS.  73 

Logs — Continued. 

Thickness  Depth 

Feet  Feet 
Grav    micaceous    shale,    some    sandstone,    some    pieces    of    yellow 

limestone 520  525 

Gray   micaceous   shale    525  530 

Gray  micaceous  shale,  and  some  sandstone    530  535 

Gray  micaceous  shale  and  some  siderite    535  540 

Gray   micaceous    shale,    some    siderite,    and   a    few    bits    of    yellow 

limestone 540  545 

Gray  sandy  shale,  some  yellow  sandstone,  bits  of  yellow  limestone 

and    pyrite     545  550 

Black  shale  with  streaks  of  pyrite,  some  siderite  concretions,  and 

bits   of  white  limestone    550  555 

Black    shale,    some     siderite     concretions,     and     white     limestone. 

Crinoid  stem  noted    555  560 

Black  shale  and  a  few  siderite   concretions    560  565 

Yellow   concretionary   limestone    and   black   shale.      Some    siderite. 

More  shale  than  limestone    565  570 

White   and  yellow  concretionary  limestone,    some   dark   shale   and 
gray    sandstone,    bits   of   pure    calcite,    and    pyrite.      More   shale 

than  limestone    570  575 

Black    carbonaceous    shale    and    coal,    some    white    limestone    and 

siderite,  and  some  bits  of  pyrite   575  580 

Dark  shale,   some  pieces  of  yellow  limestone    580  595 

Dark  shale,   few  pieces  of  yellow  limestone   and  white   sandstone, 

a  few  pieces  of  calcite    595  600 

Dark    micaceous    shale,    some    yellow    limestone,    with    layers    of 

calcite,   and   some   sandy  shale    600  605 

Gray    sandy    shale,    some    yellow    limestone,    bits    of    white    sand- 
stone   and   pyrite    605  610 

Gray  sandy  shale,  some  pieces  of  dark  limestone,  and  bits  of  pyrite  610  615 

Dark  sandy  shale,  some  pieces  of  pyrite   615  620 

Dark    gray    micaceous    shale,    some    pieces    of    yellow    limestone, 

and    siderite    concretions    620  625 

Dark   gray   shale,    some    pieces    of   yellow   limestone    and    siderite. 

A   crinoid   stem   noted    625  630 

Gray    shale    630  635 

Gray  shale,  a  few  siderite  concretions,  and  crinoid  stems 635  640 

Gray  sandy  shale,   some  yellow  limestone,   and  concretionary  car- 
bonate of  iron    640  645 

Gray  shale,  some  coal  and  siderite    645  650 

Soft  gray  shale,  some  yellow  limestone,  and  siderite 650  655 

White  limestone,   some   "clod"   and  sandstone 655  660 

Black  "clod,"  some  yellow  limestone,  and  soft  gray  shale 660  665 

"Clod,"  with  little  white  limestone  and  crinoid  stems    665  670 

"Clod,"    crinoid    stems,     and     Edmondia    (?),     with     some     white 

limestone     675  680 

Gray  shale,   yellow  limestone  and  some  "clod" 680  685 

Yellow  limestone  and  gray  sandstone,  some  concretionary  siderite 

and  gray  shale   685  590 

Soft  gray  shale,  yellow  limestone,  and  some  sandstone 690  695 

Gray   micaceous    sandy    shale,    yellow   and   white    limestone,    some 

"clod,"   and  some  pyrites    695  700 

Gray   micaceous   shale,    some   siderite,    some   white   limestone,    and 

pieces  of  calcite,  with  some  sandstone 700  705 

Gray,    sandy    shale,    some    black    shale,    and    siderite    with    a    few 

pieces    of    coal    705  710 

Gray  sandy  shale,  some  coal,  and  siderite   710  715 

Gray  sandstone  and  some  black  carbonaceous  shale    715  720 

Coal  and  some  fire  clay    720  725 

Black  shale    725  735 

Hard   black   shale    735  740 

Black  shale,  a  little  white  sandstone   740  745 

Gray  sandstone,   some   black   pyritiferous   shale,    and  yellow  lime- 
stone       745  750 

Gray  sandstone,   bits   of  yellow  limestone    750  755 

Gray   micaceous    sandstone,    some    pieces    laminated,    and    bits    of 

yellow    limestone     755  760 

Gray  shale  and  sandstone,   some  imprints  of  leaves  in   shale 760  765 

Dark    shale,    some    sandstone,    laminated    and    micaceous,    bits    of 

yellow   limestone    765  770 

Gray  micaceous  sandstone  and  dark  shale,   some  yellow  limestone  770  780 
Gray  micaceous  sandstone,   some  dark  shale,  a  few  bits  of  lime- 
stone   780  785 

Gray  micaceous  sandstone  and  some  dark  shale   785  79  0 

Dark  gray  micaceous  shale,  bits  of  yellow  limestone,   and  siderite  790  795 

Black    micaceous    shale    795  800 

Gray  shale  and  some  black  micaceous  shale   800  805 

Gray  shale,  with  some   imprints  of  vegetation    805  810 

Dark  micaceous  shale  and  some  pieces  of  yellow  limestone 810  815 

Dark  shale,   some  fragments   of  yellow  limestone 815  820 


74 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


Logs — Continued. 


Thickness 
Feet 
Gray   micaceous    sandstone,    some    shale,    bits   of    yellow   limestone 

(small)      820 

Gray  micaceous  sandstone,   a  little   shale  and  limestone 825 

Gray  sandstone,   with  concretionary   yellow  limestone 835 

Gray  sandstone,  some  yellow  limestone,  and  white  limestone,  with 

some  pieces  of  dark  limestone    840 

Gray  micaceous  sandstone,  some  gray  shale,  and  a  few  pieces  of 

yellow   limestone    845 

Dark  gray  shale,  some  gray  sandstone,  few  pieces  of  yellow  lime- 
stone,   and   yellow   calcite.      Crinoid   stems   and   a   piece   of   shell 

noted     850 

Black   shale    and   a   little   white   limestone.      Crinoid   stems   and    a 

piece  of  brachiopod  shell  noted   855 

Black    shale    and    a   little   yellow    limestone.      Piece    of    shell    and 

crinoid    stem   noted    860 

Black  shale,   few  pieces  of  yellow  and  white  limestone 865 

Black  shale,  some  concretionary  siderite,  and  bits  of  yellow  lime- 
stone   870 

Black  shale  and  some  gray   shale    875 

Black  shale,  some  siderite  and  gray  sandstone    880 

Gray  micaceous  sandstone  and  few  pieces  of  shale 885 

Gray  sandstone,  few  pieces  of  yellow  limestone,  and  dark  shale..  890 

Gray  micaceous  shale,  some  sandstone    895 

Gray  micaceous   shale    900 

Gray  micaceous  shale  and  some  dark  shale    905 

Dark   and   gray  micaceous   shale    910 

Dark  gray  shale  and  a  few  pieces  of  white  limestone 915 

Dark  gray  shale,  bits  of  limestone,   and  pyrite    920 

Black    shale    925 

Black  shale  and  some  fire  clay,  bits  of  sandstone   930 

Gray  sandstone  and  some  dark  sandy  shale   935 

Dark  sandy  shale  and  sandstone,  bits  of  yellow  limestone 940 

Dark  sandy  shale  and  sandstone    945 

Dark  shale,  some  sandy  shale   950 

Gray    micaceous    shaly    sandstone    955 

Gray  micaceous  sandy  shale  and  sandstone    960 

Gray  micaceous  shaly  sandstone,  some  black  shale    970 

Gray  micaceous  sandy  shale,  bits  of  yellow  limestone 975 

White  micaceous  sand,  a  little  dark  shale    980 

White  micaceous  sand,   some  dark  laminated  shale    985 

Gray  sandstone  and  some  dark  micaceous  shade.     Sandstone  with 

infiltered  lime,  some  pieces  of  laminated  sandstone    900 

'White   micaceous   sand,    some   dark   shale    995 

White  micaceous  sand,  little  dark  shale    1,000 

Gray  micaceous  sand    1,005 

Gray  micaceous  sandstone,  some  dark  shale   1,01 0 

Gray  micaceous  sandstone    1,015 

Gray    shale    1,025 

Dark  gray  shale    1,035 

White  micaceous  sand,  grains  mostly  from  %  to  %mm.  in  diameter  1,040 

White  micaceous   sand    1,045 

White  micaceous  sand  with  a  little  infiltered  lime 1,065 

White  micaceous  sand  with  some  infiltered  lime,  a  little  dark  shale  1,070 

Gray  micaceous  sandstone  and  shale    1,080 

White  micaceous  sand  with  some  infiltered  lime    1,085 

Yellow  micaceous  sand    1,090 

Yellow    sand    1,125 

Yellow  sand,  showing  secondary  enlargement  of  grains 1,130 

Yellow   sand    1,135 

Yellow  sand  and  some  dark  shale   1,140 

Gray  sand  with  some  secondary  enlargement  of  crystals 1,145 

White  sand,  very  fine    1,150 

White   sand    1,155 

Fine   white   sand    1,160 

White  sand  and  some  gray  shale    1,165 

Fine   white   sand    1,170 

Fine  white  sand  with  some  infiltrated  lime    1,175 

Yellow    sand     1,180 

Yellow   sand  with   infiltrated   lime    1,190 

White  sand,  grains  mostly  from   %  to   %   mm.  in  diameter 1,210 

Fine   white   sand    1,215 

White  sand,  some  grains  show  secondary  enlargement   1,230 

White    sand    1,235 

Yellowish    sand     1,280 

Yellow   sand  and  some  white  limestone    1,290 

White    limestone    and    sand    1,300 

Like  the  preceding,  but  with  more  lime    1,305 

Greenish   shale   with   some   flakes    of   mica,    some    white  and  dark 

limestone.     Some  imprints  of  leaves    1,310 


Depth 
Feet 

825 
835 
840 

845 

850 


855 

860 

865 
870 

875 
880 
885 
890 
895 
900 
905 
910 
915 
920 
925 
930 
935 
940 
945 
950 
955 
960 
970 
975 
980 
985 
990 

995 
1,000 
1,005 
1,010 
1,015 
1,025 
1,035 
1,040 
1,045 
1,065 
1,070 
1,080 
1,085 
1,090 
1,125 
1,130 
1,135 
1,140 
1,145 
1,150 
1,155 
1,160 
1,165 
1,170 
1,175 
1,180 
1,190 
1,210 
1,215 
1,230 
1,235 
1,280 
1,290 
1,300 
1,305 
1,310 

1,315 


BLATCHLEY] 


LAWRENCE   COUNTY   LOGS. 


75 


Logs — Continued. 

Thickness  Depth 

Feet  Feet 
Greenish  shale,  or  a  fire  clay,  some  limestone,  and  bits  of  pyrite. 

Imprints   of   vegetation    1,315  1,320 

Gray  sandstone,   some  pieces  of  pyrite,  and  greenish  shale  like  in 

the    preceding    1,320  1,325 

Gray  sandstone  with  some  flakes  of  mica    1,325  1,330 

A  tangled  organic  oolitic  limestone,  breccia  and  some  sandstone..  1,330  1,335 
A  tangle  of  organic  oolitic  limestone,   effervescence,   brisk.      Some 

greenish  shale  and  sand,  bits  of  pyrite   1,335  1,345 

A  tangle  organic  oolitic  limestone,   breccia,    some   pieces   of   green 

and    red    shale     1,345  1,350 

Oolitic  limestone,    some   dark   shale,    bits    of   green   and   red    shale 

and  two  pieces  of  chert   1,350  1,355 

A  tangled  organic  oolitic  limestone,  breccia,   some  black,   greenish 

and   brown   shale    1,355  1,370 

Black  shale  and  limestone,  like  that  of  the  preceding  sample 1,370  1,375 

Black  shale  and  some  oolitic  limestone,  effervescence  brisk 1,375  1,380 

Black  and  green  shale,  white  limestone   1,380  1,390 

Black  shale  and  some  sandstone    1,390  1,395 

Black  shale  and  a  little   sandstone    1,395  1,400 

Greenish  and  red  shale,  some  limestone,  effervescence  brisk.     Bits 

of   chert   and   pyrite    1,400  1,405 

Dark  shale  and  some  reddish  colored  limestone,  effervescence  brisk  1,405  1,410 

Dark  and  reddish  brown  shale,  some  gray  limestone   1,410  1,415 

Dark  shale  and  some  gray  limestone,  a  little  red  shale 1,415  1,420 

Black  shale  and  a  little  limestone   1,420  1,425 

Black  marly  shale  and  some  white  limestone.     Bits  of  pyrite  and 

red   shale    1,425  1,435 

White  limestone,  some  black  marly  shale  and  red  shale,  numerous 

crinoid    stems 1,435  1,440 

Black  shale,  some  marly  shale  and  white  limestone,  crinoid  stems 

and  pieces  of  shells   1,440  1,445 

White  limestone  and  dark   shale    1,445  1,450 

White  limestone  and  dark  shale,  some  yellow  sandstone 1,450  1,455 

Grayish   yellow    sandstone    with   infiltered    lime,    some    dark    shale 

and  white  limestone    1,455  1,470 

Gray  sandstone,  some  black  shale    1,470  1,475 

Red  shale,  some  greenish  sandstone  with  infiltered  lime  and  little 

gray    sandstone     1,475  .1,480 

Dark  sandy  calcareous  shale,  some  white  limestone  and  red  shale  1,480  1,485 

Coarse  gray  sand  and  some  black  shale    1,485  1,490 

Coarse   gray   sand    1,490  1,500 

White  sandstone  with  infiltered  lime  and  some  dark  shale 1,500  1,515 

Gray  sandstone  and  a  little  dark  shale    1,515  1,535 

Black  shale    1,535  1,550 

Black  shale,  some  yellowish  sandstone  with  infiltered  lime 1,550  1,560 

Black  shale  and  white  limestone.     A  few  fragments  of  shells 1,560  1,565 

Black  shale  and  white  sandstone,  little  limestone 1,565  1,585 

Black  shale,  white  limestone,  effervescence  brisk,  and  some  sand..  1,585  1,590 
Black   shale   and   some   white    fragmental   limestone,    crinoid    stem 

noted     1,590  1,595 

Black    shale    1,595  1,600 

Black  shale   and  a  little   limestone    1,600  1,605 

Black  shale  and  some  sandstone,  and  white  limestone 1,605  1,610 

Gray    sand,    white    limestone,    (effervescence    brisk),    and    a    little 

dark    shale    1,610  1,620 

White  limestone  and  dark  shale    1,620  1,625 

Black   shale   and  a  little  limestone    1,625  1,645 

Black  shale  and  some  limestone.     A  crinoid  stem  noted 1,645  1,650 

Black   shale  and   some   limestone    1,650  1,660 

Black  shale    1,660  1,665 

Black  and  red  shale,  some  white  limestone   1,665  1,670 

Black   shale,   some   red  shale   and  oolitic  limestone,    (effervescence 

brisk)     1,670  1,680 

Greenish  and  reddish  shale,  some  oolitic  limestone   1,680  1,685 

Greenish  shale,  some  red  shale,  and  some  oolitic  limestone 1,685  1,690 

Oolitic  limestone,  a  little  sand  and  greenish  shale   1,690  1,710 

Oolitic   limestone    1,710  1,740 

Oolitic  limestone,  little  greenish  shale  and  bits  of  pyrite 1,740  1,745 

No.  11. 

Operators — Snowden  Bros. 

Farm  and  well — Perkins,  No.  19. 

Location — SW.  *4  sec.  32,  Bridgeport  Township. 

Elevation — 529  feet. 

Thickness  Depth 

Feet  Feet 

Soil  and  slate    140  140 

Sand    45  185 


76  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no. 

Logs — Continued. 


Slate     

Sand 

Slate    , 

Limestone     

Slate    

Slate  and  shale    , 

Sandy    shale    

Slate     

Limestone     

Slate    

Limestone 

Slate    

Limestone 

Slate    

Limestone     

Slate 

Sandy   limestone    

Slate,    white    

Slate,   brown    , 

Sand   (show  of  oil,  930  to  950  feet)    

Slate,   brown    

Slate,    gray    

Sand    (water,    1,075    feet)    

Slate    

Sandy  limestone    

Slate    

Limestone     , 

Slate 

Red   rock    

Slate     

Limestone    

Slate    

Sand    , 

Limestone 

Shale     

Red  rock    

Sand    

Red  "rock 

Slate    

Limestone    

Slate     

Sand  (oil,  1,520  feet)    , 

Slate    

Limestone     

Shale     

Limestone     

Slate    

Limestone     

Slate    

Limestone    (gas,    1,654    feet)     

Sand    (oil,   1,686   to   1,696   feet)    

Limestone     

Total  depth   1,802 

No.  12. 

Operators — Bridgeport  Oil  Company. 
Farm  and  well — Willey,  No.  4. 
Location— SE.  %  sec.  30,  Petty  Township. 
Elevation — 517  feet. 

Thickness  Depth 

Feet  Feet 

Mud    and    slate     22  22 

Sand    10  32 

Slate 128  160 

Sand 20  180 

Slate    65  245 

Limestone    5  250 

Slate    25  275 

Limestone     10  285 

Red   rock    5  290 

Slate    110  400 

Limestone     5  405 

Shale     25  430 


Thickness 

Depth 

Feet 

Feet 

15 

200 

75 

275 

30 

305 

10 

315 

20 

335 

106 

441 

10 

451 

95 

536 

8 

544 

96 

640 

5 

645 

70 

715 

6 

721 

800 

5 

805 

848 

854 

864 

910 

956 

966 

1,050 

115 

1,165 

1,205 

1,215 

15 

1,230 

7 

1,237 

1,260 

1,270 

24 

1,294 

22 

1,316 

17 

1,333 

12 

1,345 

1,367 

29 

1,396 

1,407 

1,437 

1,449 

43 

1,491 

1,494 

21 

1,515 

1,533 

1,554 

13 

1,567 

7 

1,574 

1,582 

16 

1,598 

7 

1,605 

11 

1,616 

1,686 

10 

1,696 

106 

1,802 

BLATCHLEY] 


LAWRENCE   COUNTY   LOGS. 


77 


Logs — Continued. 


Coal    

Shale   

Limestone     

Slate    

Limestone     

Slate,    black    

Sand    

Slate    

Salt    sand    

Slate    

Limestone     

Slate    

Sand    (oil,   907  feet)    

Slate    

Sand    

Slate     

Sand   (oil,  972  to  983  feet)    

Slate    

Limestone   and   shale    

Limestone     

Sand    (water,   1,077   feet)    

Limestone     

Sand    (water,   1,145  to   1,195   feet)    

Limestone     

Slate    

Red  rock    

Slate    

Limestone     

Slate    

Sand    (gas,   1,335    feet)    

Limestone    

Slate    

Red   rock 

Sand   (first  pay,  1,411  feet;  best  pav,  1,416  to  1,430  feet. 

Slate    

Limestone     

Sand     

Slate    

Limestone   (gas,  1,548  feet;  best  gas,  1,630  to  1,635  feet) 

Total  depth   


Thickness 

Depth 

Feet 

Feet 

3 

433 

7 

440 

5 

445 

155 

600 

65 

665 

20 

685 

30 

715 

35 

750 

25 

775 

40 

815 

15 

830 

67 

897 

35 

932 

18 

950 

956 

8 

964 

985 

23 

1,008 

34 

1,042 

20 

1,062 

33 

1,095 

5 

1,100 

95 

1,195 

10 

1,205 

40 

1,245 

10 

1,255 

7 

1,262 

43 

1,305 

25 

1,330 

1,340 

15 

1,355 

33 

1,388 

1,395 

50 

1,445 

13 

1,458 

42 

1,500 

10 

1.510 

30 

1,540 

95 

1,635 

1,635 


No.  18. 

Operators — Snowden  Bros. 
Farm  and  well — A.  Pepple,  No.  7. 
Location — NW.  *4  sec.  30,  Petty  Township. 
Elevation— 430  feet. 


Thickness  Depth 

Feet  Feet 

Soil  and  slate   15  15 

Sand,    white     90  105 

Slate   and    shells 90  195 

Sand,    white 25  220 

Slate  and  shells   80  300 

Limestone,   gritty,   hard    10  310 

Slate,  white    40  350 

Slate  and  limestone   shells    80  430 

Sand     12  442 

Slate    108  550 

Sand     20  570 

Shale,    black    20  590 

Slate    30  620 

Sand,  white   (hole  full  of  water,  660  feet) 85  705 

Slate,  white   79  784 

Limestone,    white    2  786 

Slate,  black    29  815 

Sand,  white   (hole  full  of  water,  895  feet)    115  930 

Slate,   black   45  975 

Sand,    dark,   hard    50  1,025 

Slate,   black,   soft    25  1,050 

Sand,    white,    hard     32  1,082 

Sandy  limestone,    dark,   hard    33  1,115 

Slate,    dark    5  1,120 

Sand,   white    (water)     53  1,173 


78  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

Logs — Continued. 


Slate,    black    

Sand,    white    

Slate,    black    .  . .' 

Red   rock    

Slate,    black     

Limestone    shells,    white    

Slate,   black    

Limestone,    white    

Slate,    black    

Red   rock    

Slate  and  shale    

Limestone,  white    

Sand,  white    

Slate,    black    

Red   rock    

Sand,  white   (oil,  1,365  to  1,380  feet) 

Limestone,  gritty,  black 

Slate,    black    

Sand,    white     

Limestone,    gray    

Slate,    white    

Lirr\estone,   white    

Slate,    black    

Sandy  limestone,  white    (gas,  1,513  to  1,515  feet) 

Sand,     white     

Sandy    limestone    

Limestone,    white     

Limestone,    brown    

Sandy  limestone,  white    (green  oil,    1,603   feet)    . 
Limestone,   white    


Thickness 

Depth 

Feet 

Feet 

27 

1,200 

10 

1,210 

8 

1,218 

7 

1,225 

13 

1,238 

10 

1,248 

12 

1,260 

8 

1,268 

10 

1,278 

6 

1,284 

14 

1,298 

7 

1,305 

13 

1,318 

1,338 

22 

1,360 

1,400 

5 

1,405 

1,430 

10 

1,440 
1,450 

20 

1,470 

1  486 

17 

1,503 

1.518 

32 

1.550 

1,557 

5 

1.562 

1,580 
1,606 
1,619 

26 

Total  depth   1,619 

No.  lJf. 

Operators — Snowden  Bros. 
Farm  and  well — Vanatta,  No.  2. 
Location — NE.  14  sec.  23,  Petty  Township. 
Elevation— 430  feet. 


Clay  and  quicksand    

Slate    

Sand  (16  bailers  of  water,  160  feet)    

Slate     

Limestone     

Slate    

Sand,  hard   (water,  850  feet)    

Slate,    soft     

Sand,    hard    

Slate,    soft    

Sand,    hard    

Limestone 

Red  rock    

Slate,     soft     

Sand,    hard    

Slate    

Sand,  hard   (show  of  oil,   1,618  feet)    

Slate    

Limestone     

Slate     

Sand,   hard    (green  oil)    

Slate     

Limestone  (show  of  oil,  1,945  feet;  hole  full  of  water,  2,325  feet) 

Total  depth,  dry  well    2,590 

No.  15. 

Operators — Snowden  Bros. 
Farm  and  well — Childress,  No.  3. 
Location — SW.  %  sec.  24,  Petty  Township. 
Elevation— 440  feet. 


Thickness 

Depth 

Feet 

Feet 

75 

75 

75 

150 

50 

200 

100 

300 

30 

330 

470 

800 

50 

850 

160 

1,010 

100 

1,110 

55 

1,165 

225 

1,390 

50 

1,440 

15 

1,455 

75 

1,530 

35 

1,565 

35 

1,600 

18 

1,618 

50 

1,668 

32 

1,700 

40 

1,740 

25 

1,765 

68 

1,830 

760 

2,590 

BLATCHLEY] 


LAWRENCE   COUNTY   LOGS. 


79 


Logs — Continued. 


Quicksand     

Sand,    limestone,    and   slate    

Limestone  shells   

Slate  and  limestone  shells    

Coal   and  slate    

Slate  and  limestone   shells    

Slate,    brown 

Sandstone,  white   (25  bailers  of  water,  500  to  525  feet) 

Slate,  black    .  .  .  • 

Slate  and  limestone  shells,  white    

Coal     

Slate  and  limestone  shells    

Limestone     

Red    rock     

Slate   and   limestone   shells 

Limestone,    white     

Slate  and  limestone  shells,   black    

Sandy   limestone,   white    

Sand,  white  and  brown   (hole  full  of  water,   1,020  to  1,065   feet) 

Sandy   limestone,   brown    

Slate,    brown     

Slate,  sand,   and  shells,  white    

Limestone,    white     

Slate    

Red  rock    

Slate  and  limestone  shells,   black    

Sand    

Slate     

Red    shale    

Slate    

Sand   (small  show  of  oil,  1,520  to  1,560  feet)    

Slate,   black    

Limestone  shells,  white    

Sandy   slate,   white    

Red   rock    

Limestone,    white     

Sand,    white,    hard    (oil)     

Slate  and  limestone  shells,   black 

Limestone     

Sand  (water,  1,781  feet) 

Total  depth    


Thickness 

Depth 

Feet 

Feet 

50 

50 

220 

270 

15 

285 

135 

420 

13 

433 

52 

485 

10 

495 

35 

530 

10 

540 

95 

635 

7 

642 

133 

775 

25 

800 

10 

810 

840 

10 

850 

130 

980 

40 

1,020 

1,295 

•20 

1,315 

1,335 

55 

1,380 

1,405 

15 

1,420 

7 

1,427 

13 

1,440 

1,484 

16 

1,500 

8 

1,508 

8 

1,516 

1,570 

50 

1,620 

5 

1,625 

25 

1,650 

1,658 

8 

1,666 

1,695 

37 

1,732 

1.776 

7 

1,783 

1.783 


No.  16. 

Operators — Bridgeport  Oil  Company. 
Farm  and  well — Wood,  No.  13. 
Location — NW.  %  sec.  20,  Petty  Township. 
Elevation— 430  feet. 


Thickness  Depth 

Feet  Feet 

Gravel   and  quicksand    90  90 

Limestone     10  100 

Sand    20  120 

Slate    115  235 

Limestone    shells    5  240 

Red   rock    10  250 

Slate    20  270 

Sand 30  300 

Slate    and  limestone    390  690 

Salt  sand    \ 35  725 

Slate   and  limestone    150  875 

Sand,    broken    30  905 

Limestone  and  slate    95  1,000 

Sand     75  1,075 

Slate  and  limestone  shells 55  1,130 

Sand    100  1,230 

Limestone,    hard     15  1,245 

Slate    25  1,270 

Limestone     5  1,275 

Sand     19  1,294 

Limestone     4  1,298 

Red   rock    10  1,308 

Slate     12  1,320 

Limestone     5  1,325 

Slate     15  1,340 

Limestone     25  1,365 


80 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


Logs — Continued. 


Thickness  Depth 

Feet  Feet 

Slate    15  1,38a 

Sand    10  1,390 

Limestone 10  1,400 

Slate   and   broken   sand 80  1,480 

Limestone     10  1,490 

Slate    20  1,510 

Limestone    v...  12  1,522 

Slate  and  limestone  shells    58  1,580 

Red    rock    : 2  1,582 

Limestone     8  1,590 

Sand    (green  oil)    15  1,605 

Limestone     15  1,620 

Slate     10  1,630 

Limestone     40  1,670 

Sand    12  1,682 

Limestone,    hard     .  . 6  1,688 

Limestone,    soft    10  1,698 

Sand    (salt  water)     7  1,705 

Total  depth 1,705 

No.  11. 

Operators — Snowden  Bros. 
Farm  and  well — Vanatta,  No.  1. 
Location — NE.  *4  sec.  15,  Petty  Township. 
Elevation — 475  feet. 


Thickness  Depth 

Feet  Feet 

Sand,    dark    : 10  23 

Slate     400  423 

Slate  and  limestone   shells    50  473 

Limestone    shell,    white    8  481 

Red   slate    .' . 12  493 

Slate    125  618 

Sand    (little   water,    633    feet)     15  633 

Shell  and  slate    100  733 

Slate    150  883 

Sand,    white     20  903 

Shale,    dark     100  1,003 

Sand,  white    (water,   1,023   feet)    20  1,023 

Slate  and   limestone   shells,    dark    72  1,095 

Sand,  white   (water,   1,115   feet)    20  1,115 

Slate,    dark    77  1,192 

Sand,    light    18  1,210 

Limestone,  gray    20  1,230 

Slate,    white    85  1,315 

Sand,  white    55  1,370 

Slate    60  1,430 

Limestone,    light     20  1,450 

Slate,    dark    60  1,510 

Limestone,    light    5  1,515 

Slate,    dark    5  1,520 

Sand,    light    76  1,596 

Slate,    dark    7  1,603 

Limestone,    light    , 10  1,613 

Slate,    dark    22  1,635 

Sand,    gray    13  1,648 

Red    slate    12  1,660 

Slate,    white    18  1,678 

Limestone   shell    7  1,685 

Slate,    white     3  1,688 

Limestone,    light 22  1,710 

Slate,    light    33  1,743 

Limestone,  light 20  1,763 

Sand,    white     99  1,862 

Slate,    dark    , 6  1,868 

Limestone,   light   5  1,873 

Slate,    dark    23  1,896 

Limestone,    light    41  1,937 

Sand,   white    8  1,945 

Slate    13  1,958 

Limestone,    gray    12  1,970 

Sandy  limestone    (water,   1,970  feet)    15  1,985 

Limestone,    gray    10  1,995 

Slate,    dark 8  2,003 


BLATCHLEY] 


LAWRENCE    COUNTY    LOGS. 


81 


Logs — Continued. 


Sandy    limestone,    hard     

Limestone,  light,  hard   (water,   2,025   feet)    

Sandy  limestone,    hard    

Limestone,   gray,   hard    

Sandy  limestone,  hard   (water,  2,110  feet)    

Limestone,    gray,    hard    

Limestone,  light,  hard  (hole  full  of  water,  2,593  feet) 

Limestone,  dark,  hard   (4  bailers  of  water,   2,235  to  2,607  feet)... 

Sandy  limestone,    gray 

Limestone,   dark,   hard    

Limestone,   gray,   hard 

Limestone,    white,    hard    

Limestone,  gray,  medium  hardness.     Limestone,  gray  hard 

Total    depth     


Thickness 

Depth 

Feet 

Feet 

17 

2,020 

28 

2,048 

20 

2,068 

12 

2,080 

95 

2,175 

60 

2,235 

358 

2,593 

82 

2,675 

40 

2,715 

25 

2,740 

15 

2,755 

15 

2,770 

166 

2,936 

2,936 


No.  18. 

Operators — Snowden  Bros. 
Farm  and  well — Piper,  No.  10. 
Location — SE.  !/±  sec.  2,  Petty  Township. 
Elevation— 439  feet. 


Thickness 


Feet 


Soil,    dark    

Gravel,  light    

Mud,   dark    

Limestone,    light    

Slate,    light    

Sand,  light   (water,  295  feet)    

Limestone,    light    

Red  rock    

Sand,   white    

Slate,    dark    

Limestone   shell,    light    

Slate,    dark    

Coal 

Slate,  black   

Limestone,   light    

Sand,  light   (5  bailers  of  water,   625  feet) 

Slate  and  limestone   shells    

Sand     

Slate    

Sand,    light.   

Limestone,    light    

Red    shale    

Shells  and  slate    

Slate,   light    

Sand,    light    

Slate,    dark    

Sand,  white   (water,   931  feet)    

Limestone,    dark    

Slate,  light 

Sand,    white     • 

Slate,    black    

Sand,    light 

Slate  and  limestone  shells   

Sand,    light     

Slate  and  limestone   shells    

Slate,   light    

Limestone,    light     

Slate   and  shells,   light    

Limestone     

Slate 

Sand    

Red   rock    

Sand,  light   (show  of  oil,   1.481  feet)    

Slate,    dark    

Sand,  dark    

Slate,    dark     

Limestone,    light     

Slate,    light    " 

Limestone,  light  


25 

10 
35 

8 

172 

75 

7 
13 
30 
98 

2 
25 

3 
57 
80 
20 
25 
20 
65 
25 
20 

5 
30 
28 
17 
35 
21 

9 
20 
120 
70 
40 
70 
10 
30 
60 
15 
50 
20 

5 
25 

6 
20 
10 
19 
20 

5 


Depth 

Feet 

25 

35 

70 

78 

250 

325 

332 

345 

375 

453 

455 

480 

483' 

540 

620 

640 

665 

685 

750 

775 

795 

soo 

830 
858 
875- 
910 
931 

94a 

960 
1,080 

1,15a 
1,19a 
i,26a 

1,270 
1,300 
1,360 
1,375 
1,425 
1,445 
1,450 
1,475 
1,481 
1,501 
1.511 
1,530 
1,550 
1,555 
1,560 
1,564 


—6    G 


[BULL 

.  NO.  22 

:ness 
set 

Depth 
Feet 

27 
29 
10 
25 
40 
13 

1,591 
1,620 
1,630 
1,655 
1,695 
1,708 

82  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES. 

Logs — Concluded. 


Slate,    dark    

Sand,    light    

Slate,    light    

Limestone  shells  and  sand    

Limestone    shells    and    slate    

Limestone     

Total    depth     1,708 

STRATIGRAPHY. 

Pleistocene. 

There  is  a  varying  thickness  of  glacial  deposits  over  the  Lawrence 
county  oil  fields.  The  drift  is  from  100  to  115  feet  thick  in  the  northern 
part  of  Petty  township.  It  thins  very  rapidly  toward  the  south  boundary 
of  Petty  and  the  northern  limit  of  Bridgeport  townships,  which  is  the 
area  of  a  conspicuous  uplift  of  the  LaSalle  anticline.  The  drift  over 
this  structure  is  only  20  to  40  feet  thick.  South  of  the  uplift,  in  the 
lower  part  of  Bridgeport  and  over  the  Dennison  and  Lawrence  fields, 
the  drift  is  50  to  80  feet  thick.  It  thickens  perceptibly  westward  toward 
the  Illinois  basin. 

Pennsylvanian. 

The  Pennsylvanian  rocks  of  Lawrence  county  include  the  shallow 
producing  sand  of  lower  Dennison  township,  probably  of  McLeansboro 
age ;  the  Bridgeport  sands  in  the  upper  part  of  the  Pottsville ;  and  the 
Buchanan  sand  in  the  basal  portion  of  the  Pottsville  rocks. 

McLeansboro  and  Carbondale  Formations. 

It  is  impossible  to  find  the  top  of  the  Herrin  coal  or  the  dividing  line 
between  the  McLeansboro  and  Carbondale  formations  in  this  county. 
No  Fusulina  fossils  were  found  by  Dr.  Udden  in  the  samples  of  wells 
2,  5  and  10.  The  rocks  of  the  McLeansboro  and  Carbondale  formations 
are  similar  to  those  of  Crawford  county.  They  are  represented  mostly 
by  shales,  numerous  sandstones,  and  a  few  widely  separated  beds  of 
limestone  and  coal.  Owing  to  the  impossibility  of  tracing  individual 
horizons  through  the  section,  no  correlations  were  attempted.  A  casual 
study  of  the  Bridgeport  sands  immediately  beneath  the  Carbondale  re- 
veals a  mild  uplift  and  shows  them  to  be  influenced  by  the  LaSalle 
anticline,  though  much  less  in  extent  than  the  lower  producing  forma- 
tions. Owing  to  the  impossibility  of  wide  correlation,  through  confusion 
with  lower  Pottsville  sand  beds,  only  local  studies  could  be  made.  The 
sharply  defined  structure  of  the  Mississippian  rocks,  the  unconformity 
between  the  Pennsylvanian  and  Mississippian,  and  the  milder  folding 
of  the  Pennsylvanian  beds,  suggests  a  secondary  disturbance  in  this 
region.  The  Pennsylvanian  rocks  are  thinner  over  the  major  uplift  of 
the  anticline  which  is  probably  due  to  a  preexisting  fold  in  the  Missis- 
sippian and  to  erosion  before  becoming  drift  covered. 

Pottsville  Formation — The  Pottsville  rocks  are  mostly  the  massive 
sandstones  of  the  basal  part  of  the  Pennsylvanian.     The  sandstone  beds 


blatchley]  LAWRENCE   COUNTY    STRATIGRAPHY.  83 

are  often  separated  by  lenses  of  shale  and  contain  no  limestone.  Through 
the  section  they  are  from  290  to  600  feet  thick  with  an  average  of  395 
feet.  They  are  very  much  thinner  over  the  uplift  of  the  La  Salle  anti- 
cline than  along  less  disturbed  areas.  The  Pottsville  rocks  rest  uncom- 
fortably upon  the  Mississippian  and  therefore  show  much  irregularity 
in  thickness.  Additional  irregularity  of  the  uppermost  sands  suggest 
a  slight  uncomformity  between  the  Pottsville  and  Carbondale.  The 
Pottsville  is  a  prominent  salt  water  horizon  over  most  of  Illinois  and 
the  main  oil  fields. 

Eecords  8,  3  and  7  of  Plate  II  and  2,  5  and  18  of  Plate  IIIA,  in  addi- 
tion to  that  of  well  Pet.  Sec.  36,  S.  W.  No.  8  presented  in  the  A-A  cross- 
section  of  Lawrence  county,  page  116,  were  assembled  and  plotted  in 
Plate  IIIB  to  show  .the  relations  of  the  Robinson  and  Bridgeport  sands  to 
each  other.  The  logs  are  arranged  in  order  from  south  to  north  and  are 
plotted  with  respect  to  the  top  of  the  Pottsville  which  is  the  key  line. 
The  coal-bearing  rocks  of  the  McLeansboro  and  Carbondale  lie  above 
the  line.  The  upper  Bridgeport  sands  lie  immediately  below  the  line  in 
the  first  four  and  the  upper  Robinson  sands  in  the  last  three  logs.  Both 
the  Robinson  and  Bridgeport  lenses  are  portions  of  conspicuous  sandy 
zones,  belonging  to  the  Pottsville. 

Mississippian. 

The  Mississippian  rocks  underlie  the  Pennsylvanian  and  contain  the 
most  important  oil  sands.  The  upper  portion,  known  as  the  Chester 
group,1  is  limited  by  erosion  to  the  Tribune  formation.  Below  the 
Chester  in  succession  are  the  Ste.  Genevieve  and  St.  Louis  formations. 
The  Chester  beds  include  the  "Gas,"  Kirkwood,  and  Tracey  sands,  and 
the  Ste.  Genevieve  contains  the  rich  McClosky  sand. 

Tribune  formation  (upper  portion  of  the  Chester  group) — The 
Tribune  formation  is  characterized  by  a  succession  of  limestones  inter- 
lain  with  numerous  strata  of  sand,  and  red  shales.  The  top  of  the 
Chester  is  considered  to  be  the  first  limestone  underlying  the  Pottsville 
sandstones  or  separated  from  them  by  a  stratum  of  shale.  The  top 
limestone  varies  in  its  depth  from  the  surface  through  the  region,  which 
is  attributed  to  pre-Pennsylvanian  erosion.  The  uplift  in  southern  Petty 
and  northern  Bridgeport  townships  exposed  much  of  the  upper  portions 
of  the  Chester  to  effective  erosion.  The  average  thickness  of  the  Tribune 
formation  in  this  region  is  365  feet  with  a  range  of  295  to  -140  feet.  The 
Chester  rocks  in  southwestern  Illinois,  in  comparison,  are  about  700 
feet  thick.  There  are  two  extreme  thicknesses  of  about  410  feet  in  logs 
14  and  15.  The  wells  yielding  these  logs  are  some  distance  down  the 
western  limb  of  the  anticline  where  the  formations  thicken  as  they 
descend  into  the  Illinois  basin. 

There  are  usually  three  strata  of  limestone  interlain  with  shales  which 
are  penetrated  before  the  first  distinct  sand  is  encountered  in  the  Chester 
of  Lawrence  county.  This  sand  is  known  as  the  "Gas"  sand  and  is 
present  over  the  northern  half  of  the  county.  The  average  interval  be- 
tween the  top  limestone  of  the  Chester  and  the  "Gas"  sand  in  logs  11, 
12.  13,  15,  and  19  is  125  feet.     The  next  sand  below  the  "Gas"  sand  is 


i  By  some  geologists  the  Ste.  Genevieve  is  also  included  in  the  Chester  group. 


84  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

the  Kirkwood,  192  feet  beneath  the  top  of  the  Chester.  The  Kirkwood 
sand  is  the  most  widespread  of  all  producing  horizons  in  Illinois.  It 
usually  lies  about  the  middle  of  the  Chester  beds  of  the  main  fields. 
This  sand  is  often  divided  into  two  or  even  three  lenses. 

The  red  shales  are  prominent  horizon  markers  over  most  of  central 
and  southern  Illinois  and  the  oil  fields.  These  shales  are  usually 
very  soft  and  tend  to  discolor  the  water  in  drilling  and  thus  indicate 
their  presence.  Most  of  the  complete  records  in  Lawrence  county  show 
at  least  three  red  shales  in  the  Chester.  Two  of  these  usually  occur 
over  the  Kirkwood  and  one  beneath.  The  second  red  bed  is  often  found 
immediately  over  the  Kirkwood  sand.  The  highest  red  shale  of  the 
Chester  is  about  50  feet  below  the  top  limestone  in  the  northern  portion 
of  the  field  but  is  very  irregular  in  the  southern  division. 

The  Tracey  sand  is  about  317  feet  and  the  McClosky  of  the  Ste.  Gene- 
vieve is  446  feet  lower  than  the  top  of  the  Chester  rocks.  The  lowest 
wells  on  the  western  flank  of  the  anticline  (Nos.  14  and  17)  show  larger 
intervals  between  the  top  limestone  of  the  Chester  and  the  lower  beds 
than  other  wells  over  the  crest  of  the  fold. 

The  Tracey  sand  probably  corresponds  to  one  of  the  lower  sand  mem- 
bers of  the  Tribune  in  southwestern  Illinois.  The  formation  is  quite 
uniform  in  character,  a  moderately  fine-grained,  yellowish-brown  sand- 
stone, rather  heavily  bedded  in  its  lower  portion,  becoming  more  thinly 
bedded  above.  Its  thickness  varies  from  80  feet  or  less  to  150  feet  or 
more. 

Ste.  Genevieve — The  Ste.  Genevieve  limestone  underlies  the  Chester 
rocks.  Stuart  Weller  says  of  the  Ste.  Genevieve  i1  "The  Ste.  Genevieve 
limestone  has  usually  not  been  distinguished  from  the  St.  Louis,  and  in 
its  lithologic  characters,  especially  in  its  variability,  it  closely  resembles 
the  St.  Louis.  In  it,  however,  oolitic  beds,  which  are  absent  in  the  St. 
Louis,  appear,  and  it  is,  perhaps,  less  cherty  than  the  St.  Louis.  The 
main  distinction  is  a  faunal  one,  there  being  a  recurrence  of  the  types 
of  life  which  were  abundant  in  the  Salem,,  but  absent  from  the  St.  Louis 

Three  members  of  the  Ste.  Genevieve  limestone  have 

been  recognized  by  Ulrich,2  the  Fredonia  member  below,  the  Eosiclare 
sandstone  member  in  the  middle,  and  the  O'Hara  member,  consisting  of 
limestone  and  shale,  at  the  top.     It  is  nowhere  possible  to  draw  a  sharp 

line  between  the  St.  Louis  limestone  and  the  base  of  the  Fredonia 

......    but  the  line  between  the   Ste.   Genevieve  and  the   superjacent 

CypTess  sandstone  is  a  distinct  stratigraphic  break  marked  by  an  erosion 
unconformity. 

Dr.  Weller  has  further  observed  that  the  Ste.  Genevieve  of  western 
Illinois  is  more  oolitic  than  the  average  in  its  lower  member  and  is  con- 
spicuously cross-bedded.  Its  maximum  thickness  in  Monroe  county  is 
100  feet  with  an  average  of  about  80  feet.  He  thinks  it  is  possible  that 
the  Illinois  Ste.  Genevieve  may  represent  only  the  Fredonia  limestone  of 
Ulrich' s  interpretation. 

The  top  of  the  Ste.  Genevieve  is  used  as  a  key  line  for  the  columnar 
section  of  Lawrence  county,  because  of  its  persistance  over  the  oil  field. 
The  records  of  wells  and  observations  of  oil  men  show  this  limestone 


i  Ibid,  p.  26. 

2  Ulrich,  E.  O.,  and  Smith,  W.  S.  T.    The  lead,  zinc  and  flourspar  deposits  of  Western  Kentucky. 
Prof.  Paper  U.  S.  Ge  1.  Survey,  No.  36,  1905,  p.  38. 


BLAtchley]  LAWRENCE    COUNTY    STRATIGRAPHY.  85 

to  be  particularly  soft  in  comparison  with  the  underlying  St.  Louis  lime- 
stone. It  merges  into  the  St.  Louis  and  the  only  possible  distinction 
between  them  in  this  district  is  one  of  hardness.  The  Ste.  Genevieve  has 
an  gypTflo-A  thiHmpss  nf  &5  ia&k  avov  £ko  finm    w,-+i,  - -*  t<  ^q  -j^q 

lumnar 
.  This 
of  Illi- 
9   basal 

ven  the 
•oduced 

steady 
iuction 
pth  for 

found 

.  Gene- 
T  color, 
embers 
'he  St. 
jre  680 
)0  feet 
Dore  in 
Jo.  14, 


84  OIL  FIELDS  OF  CRAWFOED  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

the  Kirkwood,  192  feet  beneath  the  top  of  the  Chester.  The  Kirkwood 
sand  is  the  most  widespread  of  all  producing  horizons  in  Illinois.  It 
usually  lies  about  the  middle  of  the  Chester  beds  of  the  main  fields. 

This   SaiT^  ■PJ--—    'Li — l^^    i^+^   +„,^    ^v  £>v.cm    ihr&o   lpnsPS. 

The  r 
and  sov 
very  sof 
their  pr< 
at  least 
over  the 
immedia 
Chester 
of  the  fi 

The  1 
vieve  is 
wells  on 
intervals 
than  otl 

The  1 
bers  of 
uniform 
stone,  r; 
bedded 
more. 

Ste.  ' 
rocks, 
limestor 
its  litho 
the  St. 
Louis,  i 
main  di 
of  life  v 

been  re< 
sandstoi 
lime  st  oi 
line  bet 

Cypress 
unconfc 

Dr.  ^ 
Illinois 
spicuoui 
100  feei 
the  Illi] 
Ulrich'e 

The 
section 
The  rec 

i  Ibid,  p 

2  Ulrich, 

Prof.  Pape 


blatchley]  LAWRENCE   COUXTY    STRATIGRAPHY.  85 

to  be  particularly  soft  in  comparison  with  the  underlying  St.  Louis  lime- 
stone. It  merges  into  the  St.  Louis  and  the  only  possible  distinction 
between  them  in  this  district  is  one  of  hardness.  The  Ste.  Genevieve  has 
an  average  thickness  of  85  feet  over  the  held,  with  a  range  of  56  to  120 
feet. 

Dr.  Udden  studied  samples  from  wells  2,  5,  and  10  of  the  columnar 
section  and  makes  note  of  oolites  at  the  top  of  the  Ste.  Genevieve.  This 
strongly  corroborates  Mr.  Weller's  idea  that  the  Ste.  Genevieve  of  Illi- 
nois and  particularly  this  portion  of  the  State  represents  the  basal 
Fredonia. 

The  Ste.  Genevieve  contains  the  McClosky  sand,  which  has  proven  the 
most  prolific  oil  horizon  in  Illinois.  The  wells  have  not  only  produced 
an  exceptionally  large  initial  flow  but  they  have  maintained  a  steady 
yield.  They  have  been  instrumental  in  upholding  the  Illinois  production 
when  other  sections  of  the  field  were  declining.  The  range  of  depth  for 
the  productive  McClosky  sand  is  1,550  to  1,850  feet,  The  oil  is  found 
20  to  50  feet  in  the  limestone. 

St.  Louis  Formation^ — The  St.  Louis  limestone  underlies  the  Ste.  Gene- 
vieve and  is  characterized  by  extreme  hardness,-  and  a  blue-gray  color. 
It  is  often  very  cherty.  This  bed,  with  subjacent  limestone  members 
of  the  Mississippian  are  over  900  feet  thick  in  this  locality.  The  St. 
Louis  was  penetrated  in  wells  4,  7,  9,  11,  14^  and  17.  There  were  680 
feet  of  St.  Louis  and  lower  members  recorded  in  Xo.  14  and  890  feet 
in  Xo.  17.  Well  Xo.  17  of  the  columnar  section  is  the  deepest  bore  in 
Lawrence  countv.  It  is  2,936  feet  deep.  The  next  deepest  is  Xo.  14, 
2,590  feet. 


86  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


CHAPTER  II. 


General  Description  of  Features  of  the  Main  Fields. 


INTRODUCTION. 

It  is  not  the  object  of  this  report  to  outline  new  prospective  oil  areas 
but  to  present  the  geological  facts  observed  in  the  developed  fields,  that 
will  corroborate  certain  laws  governing  the  genesis  and  accumulation  of 
oil  and  gas.  Certain  facts  are  presented  showing  the  relation  of  the 
quantities  of  oil,  salt  water,  porosity  of  the  sand,  etc.,  to  the  structural 
features  of  the  sand.  The  structure  of  individual  sands  is  plotted  in 
detail  by  use  of  contours  and  cross-sections;  these  show  the  vertical 
amplitude  of  the  arches. 

FIELD  W.OEK. 
Topographic  Surveys  of  the  Area. 

The  United  States  Geological  Survey  and  the  State  Geological  Sur- 
vey in  cooperation,  have  been  making  topographic  surveys  in  and  near 
the  oil  fields.  The  Hardinville  quadrangle  survey  was  completed  in 
1908.  It  covers  an  area  17  miles  long  by  13y2  miles  wide,  south  of  the 
Illinois  Central  Railroad.  The  southern  half  of  the  Crawford  county 
oil  fields  and  the  northern  portion  of  the  Lawrence  county  fields,  namely 
that  portion  in  Petty  township,  lie  within  the  Hardinville  area.  The 
Sumner  quadrangle  adjoins  the  Hardinville  area  on  the  south  and  in- 
cludes a  small  portion  of  this  field  in  its  northeast  corner.  The  survey 
and  topographic  work  was  completed  during  the  field  season  of  1911. 
The  Vincennes  quadrangle  adjoins  the  Sumner  area  on  the  east  and 
extends  into  Indiana.  It  includes  a  large  portion  of  the  Lawrence 
county  fields  in  its  northwest  corner.  The  primary  control  has  been 
made  for  the  quadrangle  but  the  secondary  leveling  and  topographic 
work  of  the  Illinois  portion  of  the  area  are  planned  for  the  season  of 
1912.  The  levels  established  in  the  Hardinville  and  Sumner  quadrangles 
serve  as  a  basis  of  the  work  incidental  to  this  report. 

The  cooperative  work  of  both  surveys  has  been  further  extended  north 
of  the  Hardinville  sheet,  in  the  survey  and  study  of  over-flowed  lands 
along  North  Fork  of  Embarrass  river.  This  covers  a  narrow  strip  along 
the  west  side  of  the  proposed  Moonshine  quadrangle,  adjoining  the  Har- 


blatchley]  HARDINVILLE    QUADRANGLE.  87 

dinville  area  in  the  north.  The  survey  parallels  the  west  side  of  the  oil 
fields  of  Crawford  county  and  will  probably  serve  as  a  basis  for  future 
work  in  that  area.  The  proposed  Oilfield  quadrangle  is  the  second  north 
of  the  Hardinville,  and  the  first  north  of  the  Moonshine  quadrangles.  It 
is  planned  to  survey  this  area  soon.  This  will  then  serve  as  a  basis  for 
geological  study  of  the  shallow  fields  of  Clark  county. 

The  work  of  computing  the  altitudes  of  wells  and  tops  of  the  various 
producing  sands  would  not  have  been  possible  had  not  bench  marks  been 
scattered  advantageously  over  the  fields,  particularly  along  highways. 
There  were  usually  one-half  dozen  or  more  elevations  painted  on  tele- 
graph poles  and  fences  along  each  section,  which  enabled  the  field  men 
to  run  levels  to  the  wells  with  a  reasonable  degree  of  accuracy  and  at 
the  same  time  to  check  with  other  levels  on  adjoining  roads  or  in  other 
sections. 

LEVELS   IN    THE   OIL   FIELDS. 

The  primary  levels  of  the  U.  S.  Geological  Survey  are  the  most  im- 
portant in  the  oil  fields,  as  alsewhere,  since  they  are  based  upon  precise 
levels  from  a  mean  sea  level  and  hence  are  of  th  highest  order.  They  are 
usually  carried  in  circuits  and  thus  check  upon  themselves.  The  benches 
of  these  levels  are  usually  the  permanent  iron  posts  planted,  two  in 
each  township,  and  not  more  than  six  miles  apart.  The  secondary  or 
"flying"  levels  are  carried  from  the  permanent  bench  posts  and  are 
spread  generally  over  local  areas.  The  level  figures  are  painted  on 
fences,  culverts,  bridges,  telephone  posts,  etc.,  in  order  to  aid  the  topo- 
grapher and  geologist  in  contouring  and  detailed  leveling. 

The  limit  of  error  in  primary  leveling  is  about  six  inches  in  100  miles 
circuit.  There  is  no  prescribed  limit  of  error  in  secondary  leveling 
although  it  usually  is  one  foot,  which  can  be  easily  adjusted  between 
permanent  bench  marks. 

The  results  of  precise  and  primary  leveling  in  the  Hardinville  and 
Sumner  quadrangles  are  given  as  follows  i1 

Hardinville  quadrangle. 

The  elevations  in  the  following  list  are  based  upon  bench  mark  B3 
of  the  Coast  and  Geodetic  Survey  at  Olney,  111.,  a  square  cut  at  the- 
base  of  one  of  the  columns  of  the  north  face  of  the  court  house.  The 
elevation  now  accepted  is  486.117  feet  above  mean  sea  level  as  de- 
termined by  the  1907  adjustment. 

The  leveling  was  done  in  1907  by  Mr.  Henry  Bucher,  levelman. 

The  work  was  done  in  cooperation  with  the  State  and  the  bench 
marks  are  stamped  with  the  State  name. 

HICKORY  POINT  SCHOOL  ALONG  HIGHWAYS  NORTH,  TO  T.  6  N.,  R.  14  W.,  NORTHEAST 
CORNER  SECTION  10,  THENCE  EAST,  TO  T.  6  N.,  R.  12  W.,  NORTHEAST  CORNER  SEC- 
TION 7,  THENCE  NORTH,  TO  INDIANAPOLIS  SOUTHERN  RAILROAD  AND  EAST  ALONG 
LATTER    2    MILES.    TO   ROBINSON. 

Feet. 
T.  4  N.,  R.  14  W.,  0.25  mile  south  of  northwest  corner  of  section  27, 
southeast  corner  of  T  road,  on  east  side  of  road,  1.3  feet  west  of 
fence,    15    feet    south    of    fence    corner;    iron    post    stamped    "510 
ADJ"     510.502 


i  Herron,  W.  H.    Report  of  the  Cooperative  Topographic  Survey  of  Illinois,  Bull.  111.  State  Geol. 
Survey,  No.  14,  1909,  pp.  31-182. 


88  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.no.  22 

Feet 

T.  4  N.,  R.  14  W.,  southwest  corner  of  section  3,  northeast  corner 
of  crossroads,  east  side  of  road,  1.1  feet  west  of  fence,  11  feet  north 
of  fence  corner;   iron  post  stamped  "508  ADJ"   509.121 

T.  5  N.,  R.  14  W.,  northeast  corner  of  section  34,  at  southwest,  cor- 
ner of  crossroads,  on  west  side  of  road,  1.1  feet  east  of  fence,  7 
feet  south  of  fence  corner;  iron  post  stamped  "496  ADJ"  496.574 

T.  5  N.,  R.  14  W.,  southwest  corner  of  section  15,  northeast  corner 
of  crossroads,  on  north  side  of  road  near  old  rail  fence,  about  14 
feet  east  of  north  and  south  fence  line,  on  east  side  of  north  and 
south  road  (New  Light  Christian  Church  (?)  is  at  southeast 
corner  of  crossroads;    iron  post  stamped  "457  ADJ" 457.555 

T.  5  N.,  R.  14  W.,  southeast  corner  of  section  3,  northwest  corner 
of  crossroads,  west  side  of  road,  6  feet  east  of  fence  and  4  feet 
north  of  fence  corner;  iron  post  stamped  "462  ADJ"  463.263 

T.  6  N.,  R.  14  W.,  northeast  corner  of  section  27,  southwest  corner 
of  crossroads,  west  side  of  road,  1.2  feet  east  of  fence,  5.6  feet 
south  of  fence  corner;  iron  post  stamped  "483  ADJ"  . . . .' 483.969 

T.  6  N.,  R.  14  W.,  0.25  mile  east  of  southwest  corner  of  section  2, 
T  road  (the  branch  to  west  is  very  dim),  outside  of  road  at  T, 
1.3  feet  south  of  fence,  15  feet  east  of  north  and  south  fence  at 
fence  corner  (north  of  center  of  T) ;  iron  post  stamped  "478 
ADJ"     478.367 

T.  6  N.,  R.  13  W.,  northeast  corner  of  section  7,  at  southwest  corner 
of  T  road,  on  west  side  of  road,  1.2  feet  east  of  fence,  7.5  feet  south 
of  fence  corner;  iron  post  stamped  "483  ADJ" 483.298 

T.  6  N.,  R.  13  W.,  southwest  corner  of  section  2,  (crossroads)  0.75 
mile  south  of  Stoy,  on  small  bank  by  pipe  line,  1  foot  east  of  fence, 
76  feet  north  of  east  and  west  fence  line  on  north  side  of  east  and 
west  road;  iron  post  stamped  "475  ADJ"  476.261 

T.  6  N.,  R.  12  W.,  northeast  corner  of  section  7,  T  road,  on  south 
side  of  road  opposite  the  Wilson  Schoolhouse,  0.7  foot  north  of 
fence,  12  feet  east  of  fence  corner,  on  edge  of  lane  to  south;  iron 
post  stamped  "581  ADJ"   531.481 


FROM   POINT  0.75   MILE   SOUTH  OF   STOY   SOUTH   ALONG   HIGHWAYS    TO   T.    4    N.,   R.    13 
W.   NEAR  SOUTHEAST  CORNER  OF  SECTION   29. 

Feet 

T.  6  N.,  R.  13  W.,  northwest  corner  of  section  23,  T  road,  on  bank 
on  south  side  of  road  at  T,  1.5  feet  north  of  fence,  34.5  feet  east 
of  north  and  south  section  line  fence;  iron  post  stamped  "484 
ADJ"     485.269 

Hardinville,  section  34,  T.  6  N.,  R.  13  W.,  on  east  side  of  main  north 
and  south  road  just  north  of  Christian  Church,  500  feet  south  of 
crossroads,  4.2  feet  north  of  fence  line  between  McCarty  (south 
side)  and  Newman  (north  side),  6.8  feet  west  of  an  old  fence  line 
north  in  correct  position;   iron  post  stamped  "510  ADJ"   510.903 

T.  5  N.,  R.  13  W.,  0.25  mile  north  of  southwest  corner  of  section  4, 
southeast  corner  of  T  road,  at  T,  on  south  side  of  road,  0.9  feet 
north  of  fence,  39  feet  east  of  north  and  south  fence  line,  on  east 
side  of  north  and  south  road;  iron  post  stamped  "463  ADJ" 463.826 

Chauncey,  southwest  corner  of  section  28,  T.  5  N.,  R.  13  W.,  at  north- 
east corner  of  crossroads,  on  east  side  of  road,  1.2  feet  west  of 
fence,  6.6  feet  north  of  fence  corner;  iron  post  stamped  "488 
ADJ"     488.708 

T.  4  N.,  R.  13  W.,  0.25  mile  north  of  southeast  corner  of  section  8, 
northwest  corner  of  T  road,  north  side  of  road  between  2  walnut 
trees,  1.2  feet  south  of  fence,  28  feet  west  of  north  and  south 
fence  line  on  west  side  of  north  and  south  road;  iron  post  stamped 
"492    ADJ"    492.990 


blatchley]  SUMNER   QUADRANGLE.  89 

FROM    T.    6    X.,    R.    12    W.,    NORTHEAST   CORNER    OF   SECTION    29,    ALONG   HIGHWAYS 
SOUTH,    TO   FAIRVIEW   CHURCH. 

Feet. 

T.  6  N.,  R.  12  W.,  quarter  corner  east  side  of  section  29,  T  road  at 
southwest  corner,  on  south  side  of  road,  1.1  feet  north  of  fence 
7  feet  west  of  2-foot  oak  tree  at  fence  corner;  iron  post  stamped 
"512    ADJ"    512.750 

T.  5  N.,  R.  12  W.,  northwest  corner  of  section  9,  at  southeast  corner 
of  crossroads,  on  east  side  of  road,  0.8  foot  west  of  fence,  5  feet 
south  of  fence  corner;   iron  post  stamped  "523  ADJ"   . 523.318 

T.  5  N.,  R.  12  W.,  0.25  mile  east  of  northwest  corner  of  section  28, 
southeast  corner  of  crossroads,  0.8  foot  west  of  fence,  6  feet  south 
of  fence  corner;  iron  post  stamped  "442  ADJ"  442.767 

Westport,  section  32,  T.  5  N.,  R.  12  W.,  iron  truss  bridge  over  Em- 
barrass river  at  southwest  corner,  in  highest  part  of  masonry 
support,  1.  1  feet  from  east  edge,  0.3  feet  from  south  edge;  alum- 
inum tablet  stamped  "437  ADJ" 437.339 

T.  4  N.,  R.  12  W.,  northeast  corner  of  section  18,  southwest  corner 
of  crossroads,  south  side  of  road,  1.3  feet  north  of  fence,  22  feet 
west  of  north  and  south  fence  line  on  west  side  of  north  and  south 
road;  iron  post  stamped  "436  ADJ"  436.534 

T.  4  N.,  R.  12  W.,  northwest  corner  of  section  29,  at  crossroads,  on 
south  side  of  road  at  T,  2.1  feet  north  of  fence  line,  23  feet  east 
of  north  and  south  fence  line  at  fence  corner;  iron  post  stamped 
"455    ADJ" 455.678 


Su inner  quadrangle. 

The  leveling  was   done  mostly  by  H.   G.   Lowe  and  in  part  by  H. 
Bucher  in  1907. 

FROM  POINT  4  MILES  EAST  OF  OLNEY  EAST  ALONG  BALTIMORE  AND  OHIO  SOUTH- 
WESTERN RAILROAD,  TO  CLAREMONT,  THENCE  ALONG  HIGHWAYS  NORTH,  TO 
HICKORY  POINT   SCHOOL. 

(Mean  of  Direct  and  Reverse  Leveling.) 

Feet. 

Claremonc  station,  0.36  mile  west  of,  south  end  of  small  artificial 
lake,  in  top  of  east  wing  of  masonry  dam,  0.9  foot  from  west  edge 
and  1.8  feet  from  north  edge,  in  northwest  corner;  aluminum 
tablet  stamped  "498   ADJ"    498.826 

Claremont,  at  station  crossing;  top  of  south  rail   509.8 

FROM  CROSSROADS  0.93  MILE  NORTH  OF  CLAREMONT  EAST  ALONG  HIGHWAY'  TO  T 
ROAD  0.25  MILE  EAST  OF  NORTHEAST  CORNER  SECTION  5,  T.  3  N.,  R.  13  W.,  THENCE 
NORTH   1   MILE. 

Feet. 

T.  4  N.,  R.  14  W.,  southwest  corner  of  section  36,  at  northeast  corner 
of  crossroads,  on  east  side  of  road,  0.7  foot  west  of  fence,  22  feet 
north  of  fence  corner;  iron  post  stamped  "509  ADJ"  510.263 

T.  3  N.,  R.  13  W.,  0.25  mile  east  of  northwest  corner  of  section  4, 
at  T  road,  0.7  foot  north  of  fence,  24.5  feet  east  of  telegraph  pole, 
about  11  feet  east  of  center  line  of  north  and  south  road;  iron  post 
stamped    "483   ADJ"    484.085 

T.  4  N.,  R.  13  W.,  0.25  mile  east  of  northwest  corner  of  section  33, 
at  T  road,  on  west  side  of  road,  2.2  feet  east  of  fence,  in  concrete 
post  flush  with  ground;  aluminum  tablet  stamped  "Prim.  Trav. 
Sta.  No.  10,  489   ADJ"    490.408 


90  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 

FROM  T.  3  N.,  R.  13  W.,  SEC.  5,  0.25  MILE  EAST  OF  NORTHEAST  CORNER,  EAST  TO 
T.  4  N.,  R.  12  W.,  NORTHEAST  CORNER  SECTION  32,  THENCE  NORTH,  TO  FAERr 
VIEW  CHURCH. 

Feet. 

T.  4  N.,  R.  13  W.,  southwest  corner  of  section  36,  opposite  U.  B.  Union 
Chapel,  at  northeast  corner  of  crossroads,  on  east  side  of  road,  1.1 
feet  west  of  fence,  62  feet  north  of  fence;  iron  post  stamped  "570 
ADJ"     , 571.168 

T.  3  N.,  R.  12  W.,  northwest  corner  of  section  4,  at  crossroads,  State 
road  east  to  west,  on  south  side  of  road,  on  bank  a  little  east  of 
center  of  road  to  north,  0.9  foot  north  of  fence,  18.5  feet  east  of 
telegraph  pole;   iron  post  stamped  "457  ADJ"   457.461 

FROM    POINT    2    MILES    NORTH    OF    BRIDGEPORT    SOUTH,    TO    GRANT    SCHOOL,    THENCE 
WEST   5.6   MILES,   THENCE  NORTH,   TO   SUMNER. 

Feet. 

Bridgeport,  100  feet  north  of  railroad,  on  front  face  of  southeast 
corner  of  yellow  brick  building  owned  by  F.  W.  Cox,  about  3  feet 
above  sidewalk;   aluminum  tablet  stamped  "449  1908"   448.591 

T.  3  N.,  R.  12  W.,  corner  of  sections  20,  21,  28  and  29,  at  north- 
west corner  of  crossroads;  iron  post  stamped  "489  1908"   489.774 

Grant  School,  corner  of  sections  4,  5,  8  and  9,  T.  2  N.j  R.  12  W., 
at  northwest  corner  of  crossroads,  in  southeast  corner  of  school 
yard,  iron  post  stamped  "446  1908"    446.892 

T.  2  N.,  R.  13  W.,  quarter  corner  between  sections  4  and  9,  at  south- 
west corner  of  crossroads,  3  feel:  west  of  corner  of  John  White's 
yard;    iron  post  stamped  "476  1908"    477.274 

Sumner,  on  Main  street,  250  feet  south  of  railroad,  at  northeast  cor- 
ner of  street  crossing  in  brick  building  owned  by  Mart  Wagner, 
in  south  face  on  foot  from  southwest  corner  and  3  feet  above 
ground;    aluminum  tablet  stamped  "461   ILLINOIS   1908" 462.148 

Sumner,  railroad  crossing  on  Main  street;  top  of  rail  460.5 

FROM    POINT    5.6    MILES    WEST    OF    GRANT    SCHOOL    WEST,    TO    BROWNSVILLE,    THENCE 

NORTH,   TO   CLAREMONT. 

Feet. 

T.  2  N.,  Rs.  13  and  14  W.,  corner  of  sections  1,  6,  7  and  12,  Law- 
rence-Richland county  line,  at  northwest  corner  of  crossroads,  in 
root  of  tree ;    spike    537.90 

Preston  School,  corner  sections  3,  4,  9  and  10,  T.  2  N.,  R.  14  W., 
in  front  of  T  road  east,  600  feet  south  of  T  road  west,  in  south- 
east corner  of  school  yard;  iron  post  stamped  "456  1908"  456.244 

Black  Oak  School,  corner  of  sections  27,  28,  33  and  34,  T.  3  N.,  R.  14 
W.,  at  northwest  corner  of  crossroads,  in  southeast  corner  of 
school  yard,  in  tree  root;   spike   497.20 

T.  3  N.,  R.  13  W.,  at  corner  of  sections  21,  22,  27  and  28,  at  south- 
west corner  of  crossroads,  by  picket  fence;  iron  post  stamped 
"506    1908"    505.920 

Claremont,  in  front  of  station;  top  of  rail   509.7 

GRANT    SCHOOL    SOUTH,    TO    NEAR   PATTON. 

Feet. 

T.  2  N.,  R.  12  W.,  quarter  corner  between  sections  20  and  21,  at 
northeast  corner  of  crossroads,  in  southwest  corner  of  school 
yard;  iron  post  stamped  "445  1908"   445.641 

T.  1  N.,  R.  12  W.,  corner  sections  8,  9,  16  and  17,  at  northwest 
corner  of  crossroads,  by  picket  fence;  iron  post  stamped  "462 
1908"     462.325 


blatchley]  GEOGRAPHIC    POSITIONS    OF    QUADRANGLES.  91 

FROM    POINT    5.6    MILES    WEST    OF    GRANT    SCHOOL    SOUTH    AND    EAST,    VIA    FRIENDS- 

VILLE,    TO    NEAR   PATTON. 

Feet. 

T.  2  N.,  R.  13  W.,  quarter  corner  between  sections  21  and  28,  in 
front  of  T  road  west  of  schoolhouse,  4  feet  south  of  corner  fence 
post;  iron  post  stamped  "460  1908"   460.636 

Lancaster,  400  feet  east  by  400  feet  south  of  middle  of  section  4, 
T.  1  N.,  R.  13  W.,  in  west  face  of  Lutheran  church  directly  under 
window  south  of  entrance,  about  2.5  feet  above  ground;  aluminum 
table  stamped  "494  ILLINOIS  1908"    494.584 

Stoeltz  Schoolhouse,  quarter  corner  between  sections  20  and  21,  T. 
1  N.,  R.  13  W.,  at  southwest  corner  of  crossroads,  in  northeast 
corner  of  school  yard;  iron  post  stamped  "459  1908" 459.431 

Friendsville,  quarter  corner  between  sections  23  and  24,  T.  1  N., 
R.  13  W.,  in  east  side  of  brick  house  of  Dr.  C.  S.  Couch,  near 
southeast  corner,  about  3  feet  above  ground;  bronze  tablet  stamped 
"482    VIN"    481.722 


FROM    STOELTZ    SCHOOL    WEST,    TO    PINHOOK,    THENCE    NORTH,    TO    BROWNSVILLE. 

•  Feet. 

T.  1  N.,  Rs.  13  and  14  W.,  0.25  mile  north  of  quarter  corner  between 
sections  19  and  24,  in  front  of  and  about  20  feet  south  of  center 
line  of  T  road  east;   iron  post  stamped  "409  1908"  409.460 

Pinhook,  quarter  corner  between  sections  21  and  22,  T.  1  N.,  R.  14 
W.,  at  northeast  corner  of  T  road  north;  iron  post  stamped  "435 
1908"     435.611 

T.  1  and  2  N.,  R.  14  W.,  about  0.1  mile  east  of  quarter  corner  be- 
tween sections  4  and  33,  at  northwest  corner  of  crossroads,  oppo- 
site small  white  house;  iron  post  stamped  "458  1908" 458.416 

Red  Head  Schoolhouse,  quarter  corner  between  sections  16  and  21, 
T.  2  N.,  R.  14  W.,  at  southwest  corner  of  crossroads,  in  northeast 
corner  of  school  yard;  iron  post  stamped  "462  1908"  462.584 

Preston  School,  corner  of  sections  3,  4,  9  and  10,  T.  2  N.,  R.  14  W.,  in 
front  of  T  road  east,  600  feet  south  of  T  road  west,  in  south- 
east corner  of  school  yard;  iron  post  stamped  "456  1908" 456.244 


GEOGRAPHIC   POSITIONS   OE   QUADRANGLES. 

The  following  are  the  geographical  positions  of  points  in  the  three 
quadrangles  covered  by  this  report : 


Hardinville  quadrangle. 

Oraivford,  Jasper,  Lawrence  and  Richland  Counties — The  following 
geographic  positions  were  determined  by  primary  traverse  run  in  July, 
1907,  by  Mr.  J.  E.  Ellis,  assistant  topographer.  The  line  starts  from 
Claremont  triangulation  station  and  follows  highways  along  south  and 
east  edges  of  quadrangle  to  Eobinson,  thence  westerly  along  the  Illinois 
Central  Eailroad  to  Oblong  triangulation  station,  thence  westerly  along 
railroad  to  Willow  Hill,  thence  southerly  along  railroad  and  highways 
on  west  edge  of  quadrangle  to  Claremont  triangulation  station : 


92  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 

Geographic  Positions   Along  Highways   Near   South   Border   of   Quadrangle. 


Stations. 


Latitude. 


Longitude. 


Claremont  triangulation  station  of  the  U.  S.  Lake  Survey  and  U.  S. 
C.  &  G.  S.,  in  section  29,  T.  4  N.,  R.  14  W.,  German  township,  3  miles 
northwesterly  from  town  of  Claremont  a  station  on  Ohio  and  Mis- 
sissippi Railroad,  on  land  of  Brinkley  heirs.  Station  mark:  Two 
stone  posts,  one  above  the  other  in  the  usual  manner.  Reference 
marks.  One  north  67°  33'  west,  distant  23.1  meters.  One  north  0. 
39'  west,  distant  7.8  meters.  One  north  71°  45'  east,  distant  24.6 
meters  from  station  mark.  Northwest  corner  of  section  29  bears 
north  60°  03'  west,  distant  847  meters  from  station  mark 

T.  4N.,R.  14  W.,  corner  sections  28,  29,  32  and  33,  20  feet  south  to  corner 
fence  post 

T.  4  N.,  R.  14  W.,  corner  sections  27,  28,  33  and  34,  T  road  west  at  school 
house,  10  feet  east  to  rail  fence 

T.4N.,  R.  14  W.,  quarter  corner  between  sections  26  and  27,  crossroads, 
15  feet  north  to  center  of  bridge 

T.  4  N.,  R.  14  E.,  quarter  corner  between  sections  25  and  26,  center  of 
crossroads 

T.  4  N.,  R.  13  and  14  W.,  quarter  corner  between  sections  25  and  30, 
center  of  crossroads,  Richland  and  Lawrence  county  line 

Sumner,  2.25  miles  north  by  0.25  mile  west  of;  on  west  side  of  road  at 
T  road  east,  2  feet  west  to  fence,  25  feet  east  to  center  of  T  road  east, 
in  top  of  concrete  block  8  x  8  x  20"in  ground,  aluminum  tablet  stamped 
"Prim.  Trav.  Sta.  No.  10,  1907,  ILLINOIS " 

T.  4  N.,  R.  13  W:,  corner  sections  27, 28, 33  and  34, 25  feet  south  to  corner 
fence  post 

T.4N..R.13W.,  east  corner  sections  27  and  34,  stone,  T  road  west  at 
church 

T.  4  N.,  R.  13  W.,  corner  sections  25,  26,  35  and  36,  center  of  T  road 
south 

T.  4  N.,  R.  12  and  13  W.,  corner  sections  25,  30,  31  and  36,  crossroads, 
10  feet  west  to  center  of  small  bridge 

T.  4  N.,  R.  12  W.,  stone  corner  sections  29,  30,  31  and  32,  T  road  south 

Westport,  5.75  miles  due  south  of;  on  east  side  of  T  road  west  at  Fair- 
view  church,  in  top  of  concrete  block  8  x  8  x  20"  inches,  aluminum 
tablet  stamped  "Prim.  Trav.  Sta.  No.  11,  1907,  ILLINOIS" 

T.  4  N.,  R.  12  W.,  corner  sections  28,  29,  32  and  33,  center  of  T  road 
west 


38  45  28.5 

38  44  49.1 

38  44  48.8 

38  45  15.1 

38  45  14.9 

38  45  14.7 

38  44 7  47.8 

38  44  47.7 

38  44  47.5 

38  44  44.0 

38  44  43.8 

38  44  44.8 

38  44  46.0 

38  44  45.9 


87  59  40.8 

87  59  03 .2 

87  57  55.4 

87  56  47.2 

87  55  39.3 

87  54  31.4 

87  51  58.4 

87  51  06.9 

87  49  58.9 

87  48  55.7 

87  47  48.1 

87  46  42.8 

87  45  35.3 

87  45  35.5 


Geographic  Positions  Along  Highways  Near  East  Border  of  Quadrangle. 


Stations. 


Latitude.  Longitude. 


T.  4  N.,  R.  12  W.,  corner  sections  20,  21,  28  and  29,  T  road  west 

T.  4  N.,  R.  12  W.,  stone  corner  sections  16,  17,  20  and  21,  fence  east  and 

west 

Center  of  T  road  east 

T.  4  N.,  R.  12  W.,  corner  sections  7,  8,  17  and  18,  center  of  crossroads. . 

Westport,  0.75  mile  east  of;  intersection  at  T  road  west 

T.  5  N.,  R.  12  W.,  corner  sections  21,  22,  27  and  28,  center  of  county  line 
road  at  north  and  south  fence ' 

Crawford,  1  mile  north  of;  Lawrence  county  line 

T  road  east,  southeast  corner,  7  feet  north  and  4  feet  west  to  maple  tree, 
35  feet  north  and  20  feet  west  to  center  of  T  road  east,  in  concrete 
block,  aluminum  tablet  stamped  "Prim.  Trav.  Sta.  No.  12,  1907, 
ILLINOIS" 

Quarter  corner  between  sections ,  center  of  crossroads 

T.  5  and  6  N.,  R.  12  W.,  corner  sections  3,  4,  33  and  34,  stone,  1,340  feet 
east  of;  T  road  east  on  T.  S.  line 

T.  6  N.,  R.  12  W.,  corner  sections  27,  28,  33  and  34,  T  road  west,  25  feet 
due  east  to  corner  fence  post 

Road  west  at  Indian  boundary 

New  Hebron,  T  road  just  northeast  of;  10  feet  northeast  to  large  black 
oak  tree 

Lane  east  at  turn  of  road 

T.  6  N.,  R.  12  W.,  corner  sections  3,  4,  9  and  10,  T  road  west  at  school 
house,  12  feet  cast  to  corner  yard  fence 

T.  6  N.,  R.  12  W.,  north  corner  sections  3  and  4,  center  of  T  road  south, 
just  east  of  entrance  to  Robinson  Fair  Grounds 

Robinson  court  house,  in  stone  post  at  south  entrance  to  grounds, 
aluminum  tablol  stamped  "Prim.  Trav.  Sta.  No.  13,  1907,  ILLI- 
NOIS"  


38  45  39.2 

38  46  32.2 

38  46  44.2 

38  47  23.4 

38  49  40.2 

38  51  00.0 

38  51  54.8 


38  52  57.9 

38  53  40.5 

38  54  41.6 

38  55  34.0 

38  56  19.8 

38  57  31.1 

38  58  19.1 

38  58  59.3 

38  59  54.5 

39  00  IS. 2 


87  45  35.4 

87  45  35.4 

87  46  38.5 

87  46  41.8 

87  44  42.8 

87  44  26.0 

87  43  52.1 


87  43  52.7 

87  43  53.1 

87  44  10.4 

87  44  27.5 

87  44  51.8 

87  44  35.8 

87  44  30.2 

87  44  19.2 

87  44  19.8 

87  44  21.6 


BLATCHLEY] 


GEOGRAPHIC    POSITIONS    OF    QUADRANGLES. 


93 


The  following 


Sumner  quadrangle. 

Edwards,  Lawrence,  Richland  and  Wabash  Counties- 
geographic  positions  on  U.  S.  Standard  datum  were  determined  by 
primary  traverse  in  1908  by  J.  E.  Ellis,  assistant  topographer.  The 
line  starts  from  Claremont  triangulation  station  of  the  U.  S.  Lake  Sur- 
vey and  Coast  and  Geodetic  Survey  and  follows  south  along  public  high- 
ways to  Parkersburg  triangulation  station,  thence  to  southwest  corner 
of  Sumner  quadrangle,  thence  east  to  point  near  Patton  and  north  along 
border  of  quadrangle  to  primary  traverse  station  No.  11,  1907,  Illinois: 


Geographic  Positions  Along  Highways. 


Station. 

Latitude. 

Longitude. 

38 
38 

38 
38 

38 

38 
38 

38 
38 
38 
38 

38 
38 
38 
38 

38 
38 

38 
38 
38 
38 
38 
38 

38 
38 

44 

3d 

30 

30 

30 

30 
30 

35 
35 
35 
36 

37 

37 
38 
38 

39 
39 

40 
40 

41 

42 
42 
42 

43 
44 

49.2 
15.3 

15.2 
18.4 

14.6 

14.5 
10.0 

26.0 
25.7 
52.0 
44.6 

38.2 
37.5 
34.6 
34.6 

28.0 
27.7 

20.7 
20.4 
13.2 
06.2 
19.2 
59.3 

52.6 
46.0 

87 
87 

87 
87 

87 

87 
87 

87 
87 
87 
87 

87 
87 
87 
87 

87 

87 

87 
87 
87 
87 
87 
87 

87 
87 

59 
59 

57 
56 

55 

54 

47 

45 

45 
4.', 
45 

45 

4.') 
45 
45 

45 

45 

45 
45 

45 
45 
45 
45 

45 
45 

54.4 

T.  1  N.,  R.  14  W.,  1  corner  between  sees.  20  and  21,  center  of  cross  roads 

Mills  Prairie  school  house  No.  13,  at  northeast  corner  of  T  road  north, 

0.25  mile  east  of,  25  feet  south  and  25  feet  west  to  \  corner  between 

sees.  21  and  22,  T.  1  N.,  R.  14  W.,  elevation  435;  iron  post  stamped 

"Prim.  Trav.  Sta.  No.  13,  1908,  Illinois" 

05.2 

57.8 

Edwards- Wabash  county  line,  center  of  bridge  over  Bonpas  creek.. 

T.  1  N.,  R.  14  W.,  1  corner  between  sees.  23  and  24,  center  of  T  road 

south 

53.2 
48.1 

T.  1  N.,  R.  13  and  14  west,  \  corner  between  sees,  19  and  24,  center  of 
T  road  west 

41.2 

Barney  Prairie  church,  stone  at  T  road  west  at 

55.0 

Harmonv  school  house,  in  southwest  corner  of  vard  at;  35  feet  south  and 
30  feet  Vest  to  \  corner  between  sees.  20  and  31,  T.  2  N.,  R.  12  W., 
cross  roads;  elevation  445;  iron  post  stamped  "Prim.  Trav.  Sta.  No. 
17,  1908,  Illinois" 

34.1 

T.  2  N.,  R.  12  W.,  \  corner  between  sees.  20  and  21,  center  of  cross  roads 
T.  2N.,  R.  12  W.,  corner  sees.  16,  17,  20  and  21 

34.5 
34.0 

T.  2  N.,  R.  12  W.,  corner  sees.  8,  9,  16  and  17 

33.4 

Grant  school  house,  in  southeast  corner  of  vard  at;  elevation  446;  iron 
post  stamped  "Prim.  Trav.  Sta.  No.  18,  1908,  Illinois" 

33.4 

T.  2  N.,  R.  12  W.,  corner  sees.  4,  5,  8  and  9,  center  of  cross  roads 

T.  2  N.,  R.  12  W.,  corner  sees.  4  and  5  (north  corner),  T  road  south. . . 

T.  3  N,  R.  12  W.,  corner  sees.  32  and  33  (south  corner),  T  road  north.. 

Bridgeport,  at  northeast  corner  of  cross  roads  about  3  miles  south  of; 

iron  post  stamped  "Prim.  Trav.  Sta.  No.  19,  1908,  Illinois" 

33.1 
33.0 
34.6 

33.8 

T.  3  N..  R.  12  W.,  corner  sees.  28,  29,  32  and  33,  cross  roads. .   . 

34.0 

Bridgeport,  at  northwest  corner  of  cross  roads  2  miles  south  of,  eleva- 
tion 489;  iron  post  stamped  "Prim.  Trav.  Sta.  No.  20,  1908,  Illinois" 
T.  3  N,  R.  12  W.,  corner  sees.  20,  21,  28  and  29,  center  of  cross  roads... 
T.  3  N.,  R.  12  W.,  corner  sees.  16,  17,  20  and  21,  center  of  T  road  west.. 
T.  3N.,  R.  12  W.,  corner  sees.  8,9,  16  and  17 

34.3 
33.9 
33.5 
33.3 

Bridgeport,  Main  street  crossing  Baltimore  &  Ohio  railroad 

35.3 

T.  3  N.,  R.  12  W.,  corner  sees.  4,  5,  8  and  9,  center  of  cross  roads 

T.  3  N,  R.  12  W.,  corner  sees.  4  and  5  (north  corner),  20  feet  north  to  T 
road  south 

33.1 
33.0 

Westport  5.75  miles  due  south  of;  on  east  side  of  T  road  west  at  Fair- 
view  church,  in  top  of  concrete  block  8  by  8  by  20  inches;  aluminum 
tablet  stamped  "Prim.  Trav.  Sta.  No.  11,  1907,  Illinois"... 

35.3 

Magnetic  Declination  of  east  border  of  quadrangle  3°  50'  east. 
Magnetic  Declination  of  south  border  of  quadrangle  3°  47'  east. 
Magnetic  Declination  of  west  border  of  quadrangle  3°  36'  east. 


Vincennes  quadrangle. 
Geographic  Positions  Along  Highioays  Near  West  Border  of  Quadrangle. 


Station. 

Latitude. 

Longitude. 

Patton,  at  southeast  corner  of  T  road  west,  1.25  miles  north  and  0.5 
miles  east  of;  15  feet  north  and  20  feet  west  to  center  of  T  road:  iron 
post  stamped  "Prim.  Trav.  Sta.  No.  16,  1908,  Illinois" 

38    29    54.5 
38    30    34.3 
38    31    27.3 

O               1               II 

87    44    29.8 

T .  1  N .,  R.  12  W.,  corner  sees.  15,  16,  21  and  22 

87    44    30.7 

T.  1  N.,  R.  12  W.,  corner  sees.  9, 10,  15  and  16,  center  of  cross  roads 

87    44    31.8 

94  OIL  FIELDS  OF  CRAWFORD  AXD  LAWRENCE  COUNTIES,    [bull.  no.  22 

Geographic  Positions  Along  Highways  Near  South  Border  of  Quadrangle — 

Concluded. 


Stations. 


Latitude.  Longitude. 


T.  1  N.,  R.  12  W.,  corner  sees.  3,  4,  9  and  10,  center  of  T  road  west,  at 
school  house , 

T.  1  N.,  R.  12  W.,  stone  corner  sees.  3  and  4  (north  corner) 

T.  2  N.,  R.  12  W.,  stone  corner  sees.  33  and  34  (south  corner) 

T.  2  N.,  R.  12  W.,  corner  sees.  27,  28,  33  and  34,  Lawrence-Wabash 
count}'  line 

Harmony  school  house,  1  mile  east  of,  center  of  cross  roads 


38  32  20.0 

38  33  14.9 

38  33  14.9 

38  34  06.8 

38  35  25.4 


87  44  32.6 

87  44  33.4 

87  44  29.3 

87  44  28.5 

87  44  27.0 


Magnetic  Declination  west  border  of  quadrangle  3°  50'  east. 

Elevations  of  Oil  Wells. 

The  elevation  of  most  of  the  oil  wells  in  the  area  studied  were  se- 
cured by  means  of  a  Locke  or  hand-level.  The  secondary  bench  marks 
served  as  bases  for  the  work,  and  levels  were  run  from  them  to  the 
wells.  The  limit  of  error  in  this  work  was  about  two  feet,  although  it 
was  probably  less  because  of  the  check  with  previously  determined  ele- 
vations and  other  bench  marks.  Elevations  of  about  5,200  wells  were 
determined  in  the  two  counties.  The  leveling  in  the.  Hardinville  quad- 
rangle was  done  wholly  by  use  of  the  Locke  level  while  the  elevations  of 
the  wells  in  the  Sumner  quadrangle  were  determined  by  use  of  a  Y  level 
in  charge  of  W.  E.  Deuchler.  As  no  leveling  had  been  done  in  the 
Vincennes  quadrangle  it  became  necessary  to  run  secondary  levels 
through  the  active  oil  fields  from  the  Sumner  quadrangle.  About  24 
square  miles  of  secondary  levels  were  made  in  this  fashion. 

Collection  of  Well  Eecords. 

Records  were  collected  from  about  95  per  cent  of  the  wells  in  the 
area  although  about  94  per  cent  of  these  were  skeleton  logs  or  simply 
notations  of  the  depth  and  thickness  of  the  producing  sands.  The 
scarcity  of  detailed  logs  is  probably  due  to  rapidity  of  early  develop- 
ment, and  the  lack  of  appreciation  of  their  importance.  Many  detailed 
records  are  indispensable  in  a  geological  study  of  any  area,  especially 
such  as  Illinois,  which  is  so  covered  with  drift  as  to  conceal  the  se- 
quence of  formations  and  practically  all  evidence  of  folding.  Too  .little 
attention  is  paid  to  the  formations  above  the  oil  producing  sands,  which 
may  often  prove  excellent  key  horizons,  or  widespread  formations,  that 
may  enable  a  geologist  to  interpret  future  records  more  readily.  All 
operators  and  drillers  are  urged  to  note  the  positions  of  all  formations 
in  their  wells,  as  a  matter  of  possible  value  to  themselves  in  drilling  in 
other  areas  in  the  State,  and  as  an  assistance  to  the  survey  whose  duty 
it  is  to  work  out  the  geological  problems  connected  with  the  oil  industry 
of  the  State. 

The  vast  number  of  records  collected  for  study  necessitated  a  compact 
and  efficient  method  of  readily  locating  desired  logs.  A  loose-leaf  sys- 
tem was  established  for  collecting  records  in  the  field  and  later  filing 
these  permanently  in  the  office  in  suitable  binders.  The  records  are 
arranged  by  township  binders  and  in  each  of  these,  by  section,  farm 
name,  operator  and  well  number. 


BLATCHLEY]  METHODS    OF    COMPILATION    OF    REPORT.  95 

GEOLOGICAL  ASPECTS. 

General  Statement. 

It  is  particularly  valuable  if  an  area  whose  oil  resources  are  undei 
investigation  has  a  persistent  key  horizon  at  or  near  the  surface,  from 
which  may  be  determined  the  interval  to  the  producing  sands  and  the 
geologic  structure.  Coals,  such  as  the  Pittsburg  coal  of  the  Appalachian 
region  or  the  Herrin  (No.  6)  coal  of  western  Illinois,  serve  as  excellent 
key  horizons.  Limestones  of  peculiar  lithological  characteristics  are 
also  good  horizons  for  these  purposes.  Unfortunately,  the  formations 
along  the  eastern  boundary  of  Illinois,  as  over  most  of  State,  are  con- 
cealed' with  drift  and  have  been  studied  but  little.  Morever,  there  are 
no  coal  mines  in  this  section  of  the  State  and  the  wells  of  the  main  fields 
have  offered  little  or  no  help  toward  recognizing  persistent  horizons  close 
to  the  surface.  Under  these  conditions  it  became  necessary  to  resort  to 
altitudes  of  the  sand  with  respect  to  sea  level  in  the  determination  of 
structure  and  sand  relations. 

Local  Names  of  Sands. 

The  productive  horizons  in  the  several  pools  of  Lawrence  county  were 
given  the  names  of  the  land  owners  upon  whose  farms  oil  was  first  found 
in  these  particular  horizons,  except  for  the  lenticular  Bridgeport  sands, 
first  discovered  in  the  county.  These  were  named  after  the  town  of 
Bridgeport,  The  producing  sands  of  Crawford  county  are  also  lenti- 
cular and  are  called  the  Robinson  sands,  after  the  city  of  Robinson.  The 
operators  were  able  to  follow  and  distinguish  the  sands  in  their  develop- 
ment from  the  shallow  to  the  deeper  fields  and  in  computing  their 
records,  designated  the  names  of  the  sands  with  fair  accuracy.  Where 
the  names  were  missing,  the  sands  were  later  found  to  fit  their  par- 
ticular horizons  on  the  structure  maps  and  cross-sections. 

Correlation  of  Sands. 

Strip  plotting  was  resorted  to  in  correlating  sands.  The  record  of 
the  wells  were  plotted  to  uniform  scale,  and  with  the  same  symbols,  on 
long  narrow  strips  of  cross-section  paper.  The  strips  were  compared, 
and  by  shifting  one  at  the  side  of  the  others,  the  relations  of  the  logs 
to  one  another  were  found.  The  interpretation  and  correlation  of 
logs,  especially  those  of  wells  in  the  Pennsylvanian  beds,  requires  much 
work  and  the  results  are  not  always  satisfactory. 

Altitudes  of  Sands. 

The  method  used  to  ascertain  the  altitudes  of  the  tops  of  the  pro- 
ducing sands  was  to  subtract  the  elevation  of  the  mouth  of  the  well  from 
the  depth  to  the  sand.  The  altitudes  were  usually  below  sea  level  and 
therefore  were  negative.  In  drawing  a  contour  map  under  these  con- 
ditions the  high  numbers  would  signify  low  places  and  reversely,  low 
numbers  high  places.  In  order  to  avoid  confusion  in  studying  con- 
touring an  assumed  plane  1,500  feet  below  sea  level  was  chosen,  and 
from  this  the  negative  altitudes  were  subtracted.     The  resulting  high 


96  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

figures  then  correspond  to  high   places   in  the  structure   and  the   low 
numbers  to  low  places. 

Tables  of  Well  Data. 

The  desire  to  present  the  vast  amount  of  data  from  wells  in  the 
studied  area  resulted  in  the  compact  tables  presented  on  page  185. 
In  order  to  show  reference  from  well  to  table  it  became  necessary 
to  adopt  a  system  of  well  numbers  that  would  not  crowd  the  map. 
Each  section  is,  therefore,  divided  into  quarters  which  serve  as  units  for 
numbering.  The  total  number  of  wells  for  each  quarter-section  is  thus 
kept  below  100.  References  to  wells  in  the  text  are  abbreviated  as  fol- 
lows., Pet.  sec.  30,  SE.,  No.  60,  which  signifies  well  No.  60  in  the 
southeast  quarter  of  section  30,  Petty  township,  Lawrence  county,  and 
the  record  of  which  may  be  found  in  the  tables  of  well  data.  Other 
abbreviations  are  as  follows :  Ob.,  Oblong  township ;  Rob.,  Robinson 
township ;  H.  C,  Honey  creek  township ;  Mar.,  Martin  township,  all  of 
Crawford  county;  Bport.,  Bridgeport  township;  Law.,  Lawrence  town- 
ship, and  Den.,  Dennison  township,  all  of  Lawrence  county. 

Countour  Maps. 

The  structure  of  the  producing  sands  is  graphically  presented  by 
use  of  contours  or  lines  defining  the  elevation,  horizontal  form,  and 
slope  of  the  top  of  the  sand.  The  elevation  of  the  contour  is  designated 
by  the  large  number  which  is  set  in,  or  at  the  end  of,  the  line.  The 
slope,  or  dip  and  rise  of  the  sand,  is  expressed  through  numbers  on 
consecutive  contour  lines. 

The  contour  maps  were  drawn  on  a  key  or  base  map  which  shows  the 
position  and  reference  numbers  of  all  the  wells  drilled  in  the  area  and 
also  additional  culture  such  as  towns,  streams,  roads,  pumping  stations, 
etc.  All  wells  that  furnished  data  for  a  given  sand  were  plotted  in 
position  on  a  skeleton  map  on  which  the  culture  was  omitted.  The 
positive  altitudes  of  the  sands,  with  respect  to  the  assumed  datum  plane 
1,500  feet  below  mean  sea  level,  were  contoured  between  wells.  These 
constitute  the  structure  maps. 

Cross-sections. 

The  structure  of  the  several  producing  sands  is  further  shown  by 
the  use  of  cross-sections.  They  portray  graphically  the  rise  and  the 
fall  of  the  oil  sands  along  chosen  lines  and  are  intended  to  make  clearer 
the  mental  picture  of  the  contour  idea  to  those  who  are  not  familiar  with 
contouring.  At  the  same  time  the  sections  show  the  relation  of  the 
structure  of  one  sand  to  that  of  another.  The  only  cross-sections  pre- 
sented in  this  report  are  those  of  Lawrence  county. 


blatchley]  CRAWFORD    COUNTY    GEOLOGY.  97 


CHAPTER  III. 


Detailed  Geology  of  the  Crawford  County  Fields. 


GENERAL  FEATURES  OF  THE  OIL  FIELD. 

The  shape  and  extent  of  the  Crawford  county  pools  within  the  Har- 
dinville  quadrangle,  are  shown  on  Plate  IV,  the  base  map  of  the  area. 
The  map  shows  the  development  up  to  January  1,  1909.  The  Robinson 
pool  is  about  7  miles  wide  between  Oblong  and  Robinson,  but  it  narrows 
to  about  3!/2  miles  at  the  southern  limit  of  the  county.  The  western 
boundary  of  the  oil  field  trends  northwest  and  southeast  and  is  distinctly 
abrupt.  Its  eastern  edge  is  very  irregular  and  the  oil  zone  appears  to 
have  pinched  out  here  and  there  as  shown  by  light  producing  wells  and 
many  dry  holes. 

A  barren  area  about  3  miles  wide  separates  the  Robinson  and  Honey 
creek  pools  in  Crawford  county  and  continues  south  and  southwest  in 
a  Y  shape,  separating  the  Lawrence  county  pools  from  those  of  Craw- 
ford county.  Detailed  data  are  not  at  hand  to  account  definitely  for 
the  break.  It  is  probably  due  to  a  series  of  undulations  transverse  to 
the  major  axis  of  the  dominant  anticline,  since  the  Honey  creek  sands 
lie  lower  structurally  than  those  of  the  Robinson  pool  and  the  Lawrence 
county  sands,  higher  than  those  in  Crawford  county. 

Other  conspicuous  gaps  in  the  Robinson  pool  are  the  Hardinville  gas 
dome  and  an  irregular  break  from  east  to  west  directly  south  of  the 
Illinois  Central  Railroad.  The  area  just  east  of  Hardinville,  namely 
section  35,  Martin  township,  is  barren  of  oil,  except  in  the  northwest 
corner  and  along  the  south  line,  but  shows  evidence  of  fair  gas  pres- 
sures. The  producing  sands  indicate  a  structural  dome.  The  narrow 
barren  area  through  sections  2,  3,  4,  8,  9,  10  and  16,  T.  6.  N.,  R.  13 
W.,  is  due  to  noticeable  thinning  of  the  sand  which,  elsewhere,  varies 
between  2  and  15  feet  in  thickness.  In  some  instances  the  sands  are 
entirely  absent.  This  condition  is  probably  accompanied  by  a  lack  of 
sufficient  porosity  in  the  sands  to  allow  oil  diffusion ;  at  any  rate,  there 
is  more  regularity  in  the  position,  thickness,  and  production  of  the 
sands  on  both  sides  of  the  break; 

The  Crawford  county  pools  are  distinctive  for  possessing  one  general 
oil  producing  zone,  known  as  the  Robinson  sand.    This  sand  is  so  broken 

—7  G- 


98 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.' no.  22 


and  lenticular  that  it  offers  little  opportunity  for  structural  study.  In 
fact,  the  sand  shows  innumerable  streaks,  tongues,  and  detached  por- 
tions and  so  prohibits  correlation  and  contouring.  In  some  portions  of 
the  field,  however,  the  sand  is  regular  in  its  distribution.  It  is  split  into 
two  or  three  persistent  lenses  that  show  average  depths  of  about  850,900, 
and  940  feet  with  an  average  interval  between  the  tops  of  the  sands  of 
about  50  feet.  The  thickness  of  the.  sand  lenses  varies  between  2  and 
50  feet  with  an  average  of  about  25  feet.  The  average  thickness  %of  the 
lenses  is  difficult  to  estimate  because  a  great  many  wells  merely  penetrate 
the  pay  sand  and  consequently  its  total  thickness  remains  unknown. 
Beyond  the  confines  of  these  areas  the  sand  lenses  merge  into  one  an- 
other and  become  even  consolidated  in  the  wells  listed  below: 

List  of  Wells  in  Which  the  Robinson  San$  is  Exceptionally  Thick. 


Township. 

Section. 

Quarter- 
section. 

Well 
number. 

Martin 

1 

NW. 

sw. 
sw. 

NE. 

NE. 

SE. 

SW. 

SE. 

NE. 

NW. 

NW. 

SW. 

SW. 

SE. 

SE. 

NW. 

NE. 

NE. 

NW. 

SW. 

10 

1 

6 

21 

13    18 

22 

31 

23 

1 

26 

8,   13 

27 

30 

27 

18 

28 

6 

34 

1     2    5,   33 

35 

2,   5 

Honey  Creek 

6 

5 

10 

29 

3 

Oblong 

2 

1 

5 

20 

6 

6 

7 

2 

15 

31 

16 

12 

The  maximum  thickness  of 'the  consolidated  sand  lenses  is  122  feet. 
In  other  sections  of  the  field  either  one,  two,  or  even  all  the  lenses  are 
absent.     Those  wells  in  which  there  is  no  sand,  are  as  follows: 

List  of  Wells  From  Which  the  Robinson  Sand  is  Absent. 


Township. 

Section. 

Quarter- 
section. 

Well 
number. 

Oblong 

3 

SE. 

NE. 

NE. 

NW. 

NW. 

SW. 

SE. 

SE. 

SE. 

NE. 

SE. 

1 

5 

27 

8 

12 

9 

9 

18... 

1,   2 

18... 

1 

18 

2 

31 

5 

Honey  Creek 

6 

1 

22 

31 

1 

9 

The  wells  in  which  one  or  two  lenses  are  absent  are  too  numerous  to 
mention. 

There  are  additional  lenses  of  sand  both  above  and  below  the  zone 
which  includes  the  three  persistent  lenses.     One  above  is  known  as  the 


blatchley]  CRAWFORD   COUNTY   GEOLOGY.  99 

"gas"  or  ''stray"  sand.  It  is  usually  from  6  to  20  feet  thick  and  about 
20  to  50  feet  above  the  topmost  lens  of  the  Eobinson  sand.  This  sand 
produces  small  quantities  of  gas  in  portions  of  the  field,  particularly  in 
the  northern  part  of  the  Hardinville  quadrangle.  The  sand  lens  lower 
than  the  oil  zone  may  belong  to  the  Eobinson  sand  as  a  fourth  lens,  so 
closely  is  it  related  to  the  upper  lenses.  It  is  not  productive.  There  are 
other  minor  streaks  of  sand  even  in  the  producing  zone  that  add  further 
confusion  to  correlation. 

There  is  a  shallow  sand  that  is  productive  of  oil  in  section  27,  Mar- 
tin township  that  may  be  comparable  to  one  of  the  shallow  Clark  county 
sands.     Its  extent  is  very  limited. 

DETAILED  STRUCTURE  OF  THE  DISTRICT. 

Owing  to  the  irregular  deposition  of  sands  and  shales  it  was  found 
impossible  to  correlate  and  contour  any  sand  beds  definitely  except  the 
top  lens  of  the  Robinson  sand  which  is  somewhat  persistent  over  the 
area.  Even  this  work  loses  much  of  its  scientific  value  because  parts 
of  it  are  suppositional  through  the  overlapping  and  wedging  out  of 
this  sand  bed,  as  well  as  those  above  and  below  it. 

The  altitudes  of  the  top  lens  are  assembled  and  contoured  in  Plate 
5.  The  general  structure  of  the  Robinson  pool  reveals  a  broad  and 
gentle  arch  which  is  divided  into  two  parts  by  a  transverse  basin.  The 
northern  part  shows  the  arch  to  be  about  6  miles  wide  with  its  crest 
95  feet  above  the  lowest  explored  portions  of  its  limbs.  This  portion 
of  the  arch  is  subdivided  into  two  crests  of  the  same  height.  One  lies 
in  section  5  and  the  other  in  section  10,  Oblong  township.  The  southern 
portion  of  the  arch  is  about  four  miles  wide  and  110  feet  high.  The 
crest  of  this  portion  lies  in  section  35,  Martin  township.  The  two 
arches  merge  into  a  depressed  or  synclinal  area  through  sections  13,  14, 
15  and  21,  T.  6  X.,  R.  13  W.,  the  bottom  of  which  is  65  feet  lower  than 
the  crest  of  the  northern  arch  and  105  feet  lower  than  that  of  the 
southern  arch.  The  1,100-foot  contour  follows  the  limits  of  the  pool 
in  a  general  way  and  seems  to  include  most  of  the  productive  zone. 

The  contours  on  the  portion  of  the  Honey  creek  pool  shown  on  the 
map  indicate  a  lower  productive  level  than  the  Robinson  pool.  The 
heart  of  the  production  lies  along  the  1,080-foot  level  which  is  equiva- 
lent to  the  lowest  productive  levels  on  the  arch  of  the  Robinson  pool. 
This  pool  is  a  continuation  of  the  Robinson  pool  and  the  difference  in 
oil  levels  seems  to  indicate  an  intervening  depression. 

The  western  boundary  of  the  productive  field  in  Crawford  county  is 
sharply  defined  and  is  marked  by  an  abundance  of  salt  water.  It  is 
also  worthy  of  note  that  there  are  at  least  seven  wells  along  this  line 
that  show  an  absence  of  sands.  The  western  limb  of  the  arch  is  much 
the  steeper,  which  fact  corroborates  previous  observations  of  the  La- 
Salle  anticline  in  its  exposure  near  La  Salle,  111.1  It  would  then  follow 
from  the  general  knowledge  of  the  Illinois  basin2  that  the  Robinson 
sands  assume  a  much  steeper  dip  a  short  distance  west  of  the  oil  field. 
The  tendency  of  the  sands  to  remain  locally  flattened  on  the  east  side 

i  Weller,  Stuart,  The,  geological  map  of  Illinois:    Bull.  111.  State  Geol.  Survey.  No.  6,  1907,  p.  12. 
2  Oil  resources  of  Illinois  with  special  reference  to  the  area  outside  the  Southeastern  fields:    Bull.  III. 
State  Geol.  Survey,  No.  16,  1910,  pp.  48-51. 


100  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.-no.  22 

of  the  arch  is  in  keeping  with  the  slope  of  the  arch  at  LaSalle.  The 
Duncanville  and  Flat  Rock  pools  lie  at  about  the  same  general  levels 
as  the  Honey  creek  pool  and  add  further  evidence  to  the  mild  nature  of 
the  eastern  limb  of  the  anticline. 


Relations  of  Structure  to  Oil  and  Gas. 

The  Robinson  sands  have  proved  rich  in  their  yield  of  oil.  Of  the 
2,370  wells  mapped  in  this  area  but  206  or  8.7  per  cent  were  barren  of 
oil  or  gas.  The  range  of  initial  production  lies  between  1  and  about 
1,600  barrels.  The  lower  lenses  have  been  slightly  more  productive  than 
the  top  lens.  The  distribution  of  oil  has  not  been  even  over  the  area 
because  of  the  following  factors: 

1.  The  porosity  of  the  sands  is  variable  and  in  many  places  they  are 
impervious.  The  drillers  have  reported  the  sands  hard  and  dry  and 
thus  incapable  of  containing  oil. 

2.  The  sands  thin  and  thicken  commonly  and  in  some  localities 
pinch  out  altogether.  Non-porosity  usually  accompanies  such  condition. 
The  light  producing  and  barren  streak  through  sections  2,  3,  4,  9,  8  and 
7  Martin  township  offered  evidence  supporting  this. 

3.  The  sandstones  are  so  closely  interbedded  and  related  to  the 
shales  along  the  producing  zone  that  cemented  mixtures  of  the-  two 
probably  prohibit  extensive  diffusion  of  oil,  gas,  or  water  in  some  areas. 

4.  The  best  productive  areas  are  attended  with  thicknesses  between 
20  and  40  feet  of  sand  and  are  usually  free  from  large  amounts  of 
salt  water. 

5.  Local  dry  spots  in  the  midst  of  very  productive  territory  cannot 
be  attributed  to  small  depressions  or  knolls  in  the  sand  bodies  but  they 
are  explained  as  due  to  the  thinness  and  non-porosity  of  the  bed.  The 
following  few  wells  illustrate  this  fact: 

Mar.  sec.  26,  NW.  No.  4. 
Mar.  sec.  36,  SW.  No.  5. 
Ob.  sec.  15,  SE.  No.  8  and  19. 
Ob.  sec.  10,  NW.  No.  12. 
Rob.  sec.  1,  NE.  No.  7. 
H.  C.  sec.  6.  NE.  No.  11. 

The  top  lens  of  the  Robinson  sand  is  especially  rich  in  section  9  of 
Oblong,  section  6  of  Honey  creek,  and  sections  1  and  2  of  Martin  town- 
ships. The  lower  lenses  are  prolific  in  sections  21,  22,  23,  34,  and 
particularly  26  and  27,  Martin  township;  10,  14,  15  and  16,  Oblong 
township,  and  6,  10  and  15,  Honey  creek  township.  Only  about  half 
of  the  records  collected  furnished  information  of  the  initial  yield. 
Enough  data,  however,  was  gathered  to  indicate  the  distribution  of  oil 
in  the  various  sections  of  the  area.  The  following  table  shows  the  num- 
ber of  wells  that  furnished  data  of  the  production.  These  are  listed 
under  headings  of  townships,  sections,  No.  1  and  lower  lenses,  and 
initial  production.     The  gas  and  dry  wells  are  also  given: 


blatchley]  CRAWFORD   COUNTY   GEOLOGY. 

List  of  Wells  in  Craioford  County,  With  Initial  Productions. 


101 


Location. 

Number  of  wells  indicating  initial  production. 

Township. 

Section. 

Lenses. 

CO 

3 
& 

o 

6 

CO 

3 

6 

3 
8 

s 

l.O 

CO 

3 

,o 
o 

8 

o 

o 

CO 

0 

g 

1 

CO 

3 
£! 

0 

Si 

® 
> 

c 

3 

>> 

1  

No.  1 

1 
5 

2 
10 

5 
9 

4 

1 

7 
3 

1 

2 

4 
2 

1 
1 

9 
1 

1 
2 

2 

Lower 

No.  1 

2 

3 

Lower 

3 

1 

No.  1 

2 

11 

Lower 

1 

3 

No.  1 

4 

12  . 

Lower 

1 

No.  1 

1 

2 

20 

Lower 

3 

No.  1 

_ 

21 

Lower 

1 

3 

No.  1 

1 

6 

2 

12 

2 
14 

9 

1 

...... 

3 

22 

3 

6 

5 
16 

4 
12 

3 
5 

4 
4 

1 

9 

1 
2 

1 
2 

No.  1 

1 

23 

Lower 

2 

1 

6 

12 

No.  1 

1 
1 

...... 

1 

8 

24 

Lower 

7 

2 

No.l 

1 
3 

2 

25 

Lower 

1 

1 

1 

. 

No.  1 

4 

26 

1 

2 

2 
25 

2 

8 

1 
1 

7 
""18" 

""12" 

1 
3 

1 

1 
1 

4 
6 

No.  1 

1 

27 

Lower 

1 

2 

No.l 

3 

28..   . 

Lower 

2 

7 

No.  1.. 

6 

33 

Lower 

3 

1 

No.  1 

3 

34 

1 

No.l 

4 
2 

1 
3 

14 

7 

3 
5 

1 
2 

6 
4 

4 
5 

2 
6 

1 
5 

4 

35 

Lower 

No.  1 

1 

36 

2 

No.  1 

1 

1 

3 

13,19,29,32.... 
2  .   . 

2 

1 

No.  1 

6 

No.  1.. 

2 
3 

2 

1 

1 

1 
8 

2 
1 

7 
3 

4 

3  . 

Lower 

8 

1 
1 

1 

1 

1 

No.  1 

3 

4 

1 

No.  1 

, 

5  .. 

No.  1 

3 

8 

5 

6 

Lower 

2 

2 

2 

2 

No.  1 

4 

Lower 

1 

3 

102  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

List  of  Wells  in  Crawford  County,  With  Initial  Productions — Continued. 


Location. 

Number  of  wells  indicating  initial  production. 

Township. 

Section. 

Lenses. 

£1 

O 

s 

o 

s 

O 

o 

3 

o 

o 

o 

m 

o 
° 

r/2 

3 

,o 

0 
0 

>o 

6 

rn 

Q 

Oblong—  Concl'd. 

7 

No.  1 

1 

10 

9 

5 

8 

Lower 

4 
3 

2 

1 
1 

No.  1 

4 

9 

Lower 

No.  1 

1 
1 

1 
2 

10 
2 

4 
5 

8 
6 

2 
5 

7 
15 

2 
3 

2 

7 

9 

7 

1 

6 

10 

Lower 

No.  1 

1 
4 

1 
12 

3 
11 

1 
1 

1 
6 

1 
13 

1 

2 

2 

11 ,, 

No.  1 

1 

4 

1 

14 

8 

No.  1 

"""3" 

2 
13 

1 

8 

1 
3 

1 

6 

15 

Lower 

No.  1 

2 

1 

1 

3 

16 

Lower . . . 

No.  1 

5 

17 

Lower 

5 

2 
2 

10 

2 

No.  1 

3 
1 

7 

18... 

No.  1 

4 

31 

2 

8 

5 
2 

1 
1 

• 

No.  1.. 

2 

32  . 

1 

1 
2 

4 

No.  1   . 

1 
3 

1 
2 

4 

3 

3 

33 

No.  1 

2 

1 

1 

2 

2 

34 

No.  1 

3 

35 

1 

3 
1 

No.  1 

2 

3 
4 

1 

1,  11    . 

No.  1    . 

3 

1 

No.  1 

1 

1 
1 

1 

6 

1 

4 

6 

No.  1 

1 

7 

12... 

2 



No.  1 

1 

2 

3 

13 

No.  1 

1 

36 

1 
1 

No.  1 

11 

2 
2 

3 

4,  5,  7,  8,  9,  10, 
16,  17,  18,  31, 
32,33 

5 

No  1 

13 

Honey  Creek 

No.  1 

1 

4 

Lower 

1 

2 

blatchley]  CRAWFORD    COUNTY   GEOLOGY.  103 

List  of  Wells  in  Crawford  County,  With  Initial  Productions — Concluded. 


Location. 

Number  of  wells  indicating  initial  production. 

Township. 

Section. 

Lenses. 

s 

3 

o 

1 

3 

fii 

o 
a 

o 

o 
o 

!M 
C 

o 

c 
o 

3 

& 

o 

t-i 
(C 

Q 

c 

>> 

Honey  Creek- 

6 

No.  1 

3 
3 

1 

5 
5 

...... 

1 

1 

1 

3 
3 

4 

1 

1 

1 

1 

2 

..... 

8 

10          

Lower 

No.  1 

2 

15 

Lower 

No.  1 

4 

1 

1 

16 

No.  1 

1 
1 

4 
3 

4 
17 

1 

2 

31 

No.  1... 

2 
6 

1 

4 

32 

7 

No.  1.. 

2 

8 

2,  3,  7,  8,  9,  17, 
18,  19,  20,  28, 
29,30,33,34.. 

Total 

4 

3 

1 

No.  1 

17 

16 

No.  1 

27 
71 

130 
221 

64 
142 

131 

46 

32 
63 

13 
33 

42 

206 

Lower 

In  general  throughout  the  field  gas  occurs  with  oil,  but  not  in  large 
quantities.  The  wells  yielded  enough  for  use  on  the  leases  and  often 
for  drilling  but  not  for  commercial  use.  The  thin  stray  lens  above  the 
No.  1  yielded  abundant  gas,  particularly  in  the  northwest  corner  of 
Honey  creek  township.  The  quantities  were  from  1?0007000  to 
4,000,000  cubic  feet  daily  and  under  pressures  from  200  to  400  pounds 
to  the  square  inch.  These  wells  are  connected  to  large  mains  and  fur- 
nish gas  to  nearby  towns.  This  same  lens  is  productive  of  less  quanti- 
ties of  gas  in  sections  2  and  35,  Oblong  township  and  36  and  1,  Eobin- 
son  township. 

The  contours  of  the  No.l  lens  reveals  a  small  dome  on  the  anticline 
in  section  35,  Martin  township.  Several  small  gas  wells  lie  about  25 
feet  down  from  the  crest  of  the  arch  or  within  the  1,160-foot  contour. 
It  is  true  that  in  Crawford  county,  as  well  as  in  Lawrence  county,  the 
best  gas  wells  are  not  necessarily  found  on  the  highest  points  of  the 
arch  but  are  located  on  its  slopes.  Since  the  oil  lies  lower  structurally 
than  the  gas,  the  same  would  follow  for  the  oil  accumulation.  This 
would  perhaps  suggest  that  where  the  crests  of  anticlines  are  known  in 
unproven  areas,  drilling  should  be  started  slightly  to  either  side  of  the 
highest  point. 

Eelations  of  Salt  Water  to  Structure. 

The  oil  field  shows  salt  water  at  many  points,  but  particularly  along 
its  western  limit.    Water  does  not  uniformly  fill  the  rocks  of  the  region, 


104  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

as  there  are  many  dry  strata,  of  which  some  are  capable  of  containing 
water.  Great  quantities  of  salt  water  occur  upon  the  limbs  of  the  anti- 
cline and  in  the  Illinois  basin  beyond  the  productive  area  and  at  its 
sharply  defined  boundaries.  All  the  lenses  of  the  Eobinson  sand  are 
well  saturated  along  this  line,  but  the  upper  lenses  are  generally  barren 
of  water  within  the  oil  pool.  The  lower  lenses  reveal  water  across  the 
fold  and  in  some  portions  under  the  oil.  Drilling  has  proven  that  the 
oil  lies  near  the  top  of  the  lower  sand  lenses  and  consequently  but  few 
wells  pass  through  the  oil  stratum  and  into  the  water  for  fear  of  drown- 
ing out  the  oil.  The  water  is  generally  very  abundant  and  seems  to  be 
under  pressure.  Its  release  from  the  sand  sets  up  a  very  rapid  flow 
that  is  difficult  to  stop. 

The  basin  which  divides  the  major  arch  in  the  Eobinson  pool  is  barren 
of  water  but  is  productive  of  oil.  This  corroborates  the  theory  as  to  the 
accumulation  of  oil  in  dry  rocks.  The  first  lens,  however,  is  less  pro- 
ductive than  the  lower  ones  through  this  basin. 

The  trough  that  separates  the  Honey  creek  and  Robinson  pools  shows 
salt  water  in  the  scattered  dry  wells  drilled  into  it.  Most  of  the  wells 
in  the  portion  of  the  Honey  creek  pool  included  in  this  report  were 
only  drilled  into  the  oil  pay.  The  wells  that  penetrated  beneath  the  pay 
tapped  the  salt  water  zone  which  would  indicate  that  the  water  con- 
trols the  accumulation  of  the  oil  and  instrumental  in  holding  it  captive 
in  its  present  position. 

The  eastern  side  of  the  oil  field  also  shows  abundant  water  in  the 
lower  lens  but  apparently  not  so  much  as  at  the  corresponding  level  on 
the  steeper  limb  of  the  arch.  Both  water  and  oil  are  irregularly  distri- 
buted on  the  east  limb  of  the  anticline. 

Conclusion. 

It  is  obvious  from  the  position  of  the  water  and  oil  along  the  LaSalle 
anticline  that  the  water  has  controlled  the  accumulation  of  oil  in  the 
arch.  The  water  probably  has  been  a  means  of  originally  collecting  and 
causing  the  oil  to  migrate  from  long  distances  up  the  slope  of  the  arch 
and  into  its  crest.  This  is  effective  for  all  lenses  of  the  Robinson  sand. 
The  degree  of  saturation  is  variable  over  the  crest  of  the  arch.  The 
lower  lenses  are  frequently  reported  saturated  with  water  through  the 
field  whereas,  for  the  most  part,  the  upper  lens  shows  little  saturation. 


blatchley]  LAWREXCE    C0UXTY    GEOLOGY.  105 


CHAPTER  IV. 


Detailed  Geology  of  the  Lawrence  County  Field. 


GENERAL  FEATURES  OF  THE  OIL  FIELD. 

The  shape  and  extent  of  the  oil  field  in  Lawrence  county  is  shown  in 
Plate  VI,  the  base  map  of  the  area.  The  development  is  indicated  to 
July  1,  1911.  The  field  has  a  northwest  and  southeast  trend  with  its 
northern  limit  exactly  on  the  Lawrence-Crawford  county  line  and  its 
southern-most  extremity  in  sections  11  and  12,  T.  2  IS.,  R.  12  W.  The 
pool  is  continuous  for  17  miles,  although  it  is  thinly  developed  at  both 
ends.  It  is  about  2y2  miles  wide  from  the  county  line  to  about  9  miles 
south.  It  then  broadens  and  includes  the  Dennison  township  fields  in 
a  width  of  about  5  miles  and  narrows  again  at  the  extreme  southern  end 
to  about  3  miles.  The  field  changes  its  course  on  the  vicinity  of  Bridge- 
port from  about  north  24  degrees  west  to  north  44  degrees  west,  or  20 
degrees. 

The  western  edge  of  the  oil  field  is  similar  in  character  to  that  of 
Crawford  county,  in  that  it  is  almost  abrupt  and  uniform,  except  for  a 
small  detached  area  in  sections  20,  29  and  30,  Bridgeport  township. 
This  extension  of  the  field  is  due  to  a  small  terrace  on  the  western  slope 
of  the  anticline,  indicated  later  in  one  of  the  cross-sections.  The 
eastern  edge  of  the  field,  like  that  of  Crawford  county,  is  very  irregular 
and  is  probably  due  to  the  flattening  of  that  side. 

The  Lawrence  county  field  is  the  richest  of  the  eastern  Illinois  fields. 
It  has  produced  more  large  wells  than  the  rest  of  the  fields  combined 
and  its  wells  have  maintained  steadier  production  than  those  of  any 
other  locality  in  the  State.  This  field  is  prominent  because  of  its  large 
number  of  producing  sands  ranging  in  depth  from  800  to  1,900  feet, 
or  from  the  top  of  the  Pottsville  rocks  in  the  Pennsylvanian  series  to 
the  top  of  the  hard  and  thick  St.  Louis  limestone  of  the  Mississippian 
series.  There  is  a  shallow  sand  at  about  450  feet  that  produces  oil  but 
its  distribution  is  limited  to  a  very  small  area  in  sections  2  and  3, 
Dennison  township.  The  other  producing  sands  are  in  order  of  depth, 
the  three  Bridgeport  lenses,  Buchanan,  "Gas,"  Kirkwood,  Tracey  and 
McCloskv  sands. 


106  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE   COUNTIES.,  [bull.  no.  22 

DETAILED  STRUCTURE  OF  THE  DISTRICT. 

The  "Shallow"  Sand. 

A  shallow  sand  is  productive  in  sections  2  and  3,  T.  2  N.,  R.  12  W. 
It  lies  at  a  depth  of  from  444  to  485  feet  or  from  25  feet  above  sea 
level  to  about  17  feet  below.  The  initial  production  was  light,  aver- 
aging about  12  barrels  per  day.  This  sand  is  thought  to  be  the  equiva- 
lent of  a  shallow  sand  in  section  27,  Martin  township,  Crawford  county 
and  possibly  of  one  of  the  Clark  county  sands.  Further  details  of  the 
sand  are  found  in  the  tables  of  well  data. 

Bridgeport  Sand. 

The  Bridgeport  sand  derived  its  name  from  the  town  of  Bridgeport 
near  the  middle  of  the  Lawrence  county  field.  The  first  well  in  this 
field  and  in  this  sand  was  drilled  by  the  Big  Four  Oil  Company  in  July, 
1906,  on  a  narrow  strip  of  land  north  of  the  Baltimore,.  Ohio  and 
Southwestern  Railroad  and  south  of  the  public  road  in  Bridgeport.  At 
the  same  time  that  the  well  was  drilled  the  land  belonged  to  the  town  of 
Bridgeport. 

The  Bridgeport  sand  is  widely  developed  both  north  and  south  of  the 
town.  The  initial  productions  of  the  sand  are  good.  This  fact,  to- 
gether with  the  shallow  depth  at  which  the  oil  is  found,  attracted  atten- 
tion to  the  field  as  a  very  promising  area  for  exploration.  The  sand  is 
found  over  the  whole  field  but  is  especially  productive  of  oil  in  sections 
31,  32,  5,  6,  7,  8  and  17,  Bridgeport  township.  It  is  productive  of 
good  pressures  of  gas  and  some  oil  in  sections  34,  35,  3  and  2,  Dennison 
township. 

The  Bridgeport  sand  is  lenticular  and  closely  resembles  the  Robinson 
sand.  In  fact  it  seems  to  correspond  to  that  sand  in  position  and 
physical  features  as  shown  in  the  discussion  of  the  stratigraphy  of  the 
two  counties,  page  83.  This  sand  comprises  three  general  lenses  and 
some  smaller  ones  in  several  parts  of  the  oil  field.  The  depths  of  the 
sands  vary  between  600  and  1,000  feet.  Thus  a  range  of  depth  is  due 
to  a  sharp  uplift  of  the  LaSalle  anticline  and  to  the  irregularity  in  the 
surface.  It  is  impossible  to  average  the  thickness  of  the  lenses  for  the 
whole  of  the  county,  so  great  is  their  variability.  Some  of  the  lenses 
are  but  a  few  feet  thick  and  others  are  over  300  feet  through.  North  of 
Bridgeport  they  average  about  35  feet.  In  the  other  areas  of  good  pro- 
duction, the  pay  lenses  have  a  wide  range  of  thickness.  It  is  also  im- 
possible to  average  the  interval  between  lenses  because  of  the  wide 
difference  over  the  field.  The  records  in  many  instances  show  that  the 
lower  lenses  of  the  Bridgeport  sand  merge  into  the  massive  sandstone 
that  is  characteristic  of  the  Buchanan  or  basal  portion  of  the  Pottsville 
rocks. 

No  attempt  was  made  to  show  the  structure  of  this  horizon  by  means 
of  contours  or  cross-sections  because  of  the  uncertainty  of  correlation. 
Moreover  the  lack  of  sufficient  detailed  logs  also  prohibited  any  general 
conclusions  as  to  the  distribution  of  the  sand.  The  oil  and  salt  water 
relations  are  discussed  later. 


blatchley]  LAWRENCE    COUNTY   GEOLOGY.  107 

Buchanan  Sand. 

The  Buchanan  sand  is  the  next  producing  sand  lower  than  the  Bridge- 
port. It  was  first  discovered  in  September,  1906,  by  the  Ohio  Oil 
Company  on  the  E.  0.  Buchanan  farm  in  the  S.  y2  S.  E.  ^4  Sec.  16, 
Lawrence  township.  The  pay  was  found  at  1,332  feet.  The  type  area 
for  the  sand  lies  in  sections  15  and  16  Lawrence  township;  sections  21 
and  a  portion  of  22,  Dennison  township;  and  sections  17  and  20  of 
Bridgeport  township.  Data  of  the  sand  are  very  scattered  over  the 
rest  of  the  field.  There  are  enough  facts  known,  however,  to  show  the 
general  structure  up  to  and  including  sections  24,  19  and  20,  Petty 
township.  The  information  north  of  these  sections  is  scant  and  un- 
reliable because  of  the  association  of  the  Buchanan  sand  with  the  upper 
Bridgeport  lenses. 

The  Buchanan  sand  comprises  the  basal  part  of  the  Pottsville  rocks 
and  is  characterized  by  thick  or  massive  sandstones  over  most  of  Illi- 
nois. These  rocks  mark  the  lowest  portion  of  the  Pennsylvanian  series 
and  lie  unconformably  on  the  Chester  or  upper  division  of  the  Missis- 
sippian  rocks.  Most  of  the  well  data  in  the  tables  indicate  shallow 
penetration  into  this  sand,  which  was  tapped  and  entered  a  short  dis- 
tance in  order  to  provide  for  a  sufficient  and  safe  shot.  The  oil  zone 
is  usually  underlain  with  salt  water,  which,  if  tapped,  offers  danger  of 
drowning  the  oil.  In  some  localities  of  the  State  this  sand  is  called  the 
"Salt  sand"  because  saturated  with  salt  water.  This  sand  has  been  one 
of  the  most  prolific  producers  of  oil  in  the  Illinois  fields.  Its  wells  have 
yielded  large  quantities  of  oil  and  but  little  gas. 


DETAILED  STRUCTURE. 

The  altitudes  of  the  top  of  the  Buchanan  sand  were  assembled  and 
contoured  in  Plate  VII.  In  some  localities  of  the  field  wells  giving  data 
were  so  far  apart  that  it  was  not  justifiable  to  draw  definite  contour 
lines.  The  dashed  lines  were  substituted  to  indicate  the  approximate 
structure. 

The  general  structure  of  the  Buchanan  sand  reveals  a  very  irregular 
surface.  The  type  area  of  the  sand  is  the  most  completely  drilled. 
Data  from  this  locality  shows  two  small,  symmetrical,  domes,  one  in 
section  17,  Bridgeport  township  and  the  other  in  sections  15  and  16, 
Lawrence  township  and  section  21,  Dennison  township.  The  west 
dome  (section  17)  is  107  feet  high.  It  is  enclosed  by  the  640-foot 
contour  line  and  covers  about  l1/^  square  miles.  The  crest  of  the  dome 
lies  in  the  SW.  cor.,  NE.  %  sec.  17.  The  second  dome  is  99  feet 
high  and  is  also  enclosed  by  the  640-foot  contour.  It  covers  about  2 
square  miles  of  area.  Its  crest  lies  along  the  W.  %  SW.  %  sec.  15, 
Lawrence  township. 

The  sand  dips  rapidly  from  the  first  dome  in  the  type  area  toward 
the  southwest.  From  the  crest  of  this  dome  to  Bport,,  sec.  30  SE., 
No.  3,  the  clip  is  262  feet  in  about  2V2  miles  or  at  the  rate  of  105  feet 
per  mile.  This  rapid  dip  merges  into  a  minor  terrace  in  the  lower  sands 
in  the  NW.  cor.,  sec.  29,  but  is  not  shown  for  the  Buchanan  sand. 

The  structure  is  very  irregular  east  and  south  of  the  type  area  of  the 
Buchanan  sand.    The  contours  range  from  600  to  760  feet.     They  show 


108  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

a  general  dip  to  the  east.  The  west  side  of  this  part  of  the  field  is 
high  structurally  but  unproductive. 

The  Buchanan  sand  dips  sharply  north  of  the  type  area  and  then 
gradually  rises  into  an  uplift  of  the  main  axis  of  the  LaSalle  anticline 
that  has  the  appearance  of  a  narrow  double  plunging  anticline.  The 
apex  of  this  dome-like  structure  lies  near  the  center  of  section  30, 
Petty  township.  The  rise  to  the  north  from  Bport.,  sec.  17,  NE., 
No.  15  to  Pet.  sec.  30,  SE,,  No.  66  is  368  feet  in  3%  miles,  or  at  the 
rate  of  108  feet  per  mile.  The  sides  of  the  dome  dip  very  steep  to  the 
west  and  east  from  its  apex,  with  the  steeper  slope  to  the  west.  The 
dip  along  the  C-C  cross-section  from  Pet.  sec.  30,  SE.,  No.  66  to 
Bport,  sec.  36,  SE.,  No.  3  is  328  feet  in  1%  miles,  or  at  the  rate  of 
about  290  feet  per  mile.  The  dip  east  from  the  crest  of  the  dome  to 
Pet.  sec.  20,  SE.,  No.  7  along  the  same  cross-section  is  223  feet  in 
l1/^  miles,  or  at  the  rate  of  178  feet  per  mile.  The  western  side  of  the 
dome  dips  112  feet  more  per  mile  than  the  eastern  side.  This  is  in 
keeping  with  the  nature  of  the  LaSalle  fold  exposed  near  LaSalle.  The 
structure  contours  reveal  a  rapid  plunge  of  the  sand  from  the  dome  to 
the  north  and  then  a  rise  into  a  second  dome  with  a  crest  22  feet  lower 
than  the  major  uplift.  The  dip  from  the  crest  of  the  first  dome  to 
Pet.  sec.  30,  NE.,  No.  22,  at  the  bottom  of  the  basin,  is  123  feet  in 
about  one-half  of  a  mile.  The  rise  from  the  bottom  of  the  basin  to 
Pet.  sec.  19,  SE.,  No.  38,  the  crest  of  the  second  dome,  is  101  feet  in 
about  three-fourths  of  a  mile.  The  contours  indicate  a  uniform  dip 
northward  from  the  second  dome.  The  dip  of  this  sand  along  the 
western  side  of  the  anticline  is  uniform. 

A  small  though  conspicuous  terrace  interrupts  the  long  sweeping 
rise  from  the  type  area  of  the  Buchanan  sand  into  the  dome  in  Petty 
township.  It  lies  in  sections  7  and  8,  Bridgeport  township  along  the 
700-foot  contour.  The  area  covers  about  one-half  of  a  square  mile. 
The  wells  yielded  good  intial  productions  of  oil. 


"Gas"  Sand. 

The  "Gas"  sand  is  so  named  because  it  produces  small  amounts  of 
gas  wherever  encountered,  though  in  some  instances  it  is  productive  of 
oil.  The  sand  underlies  the  Buchanan  sand  and  is  usually  the  first  or 
second  sand  in  this  district  penetrated  in  the  Mississippian  or,  speci- 
fically, the  Chester  rocks.  There  are  36  wells  in  the  area  that  furnish 
data  for  both  Buchanan  and  "Gas"  sands  and  from  these  the  average 
interval  between  these  sands  is  found  to  be  198  feet. 

The  sand  is  definitely  correlated  from  section  36,  Petty  township  to 
sections  5  and  6,  Bridgeport  township.  Without  detailed  knowledge 
of  the  plunging  anticline,  in  section  30,  Petty  township  or  the  strati- 
graphy of  the  area,  the  oil  men  have  confused  the  "Gas"  sand  with  the 
upper  sands,  particularly  with  the  Buchanan  bed,  and  in  some  instances 
with  the  Kirkwood  sand  beneath.  The  relations  of  this  sand  to  the 
others  of  the  region  are  geographically  shown  in  cross-sections  A- A, 
B-B,  and  C-C. 

The  average  thickness  of  the  "Gas"  sand  estimated  from  data  fur- 
nished by  245  wells  is  16  feet  with  a  range  from  1  to  68  feet. 


blatchley]  LAWRENCE   COUNTY   GEOLOGY.  109 

The  "Gas"  sand  produces  gas  over  most  of  the  contoured  area.  The 
amounts  were  not  reported. 

DETAILED  STRUCTURE, 

The  altitudes  of  the  top  of  the  "Gas"  sand  were  assembled  and  con- 
toured in  Plate  VIII.  The  structure  of  this  sand  is  the  most  regular  of 
any  in  this  field,  with  the  exception  of  the  Kirkwood.  The  contours 
indicate  a  uniform  dip  of  the  sand  along  the  east  and  west  flanks  of  a 
strongly  defined  anticline.  The  structure  further  confirms  the  double 
plunging  of  the  major  fold  both  to  the  north  and  south.  The  highest 
point  of  the  anticlinal  dome  is  in  Pet,  sec.  30,  NE.,  No.  5.  The  dip  to 
the  north  from  this  point  to  Pet,  sec.  36,  NW.,  No.  12,  is  232  feet  in 
slightly  over  5  miles  or  at  the  rate  of  about  46  feet  per  mile.  The 
decline  to  Bport,  sec.  17,  NE.,  No.  39,  is  246  feet  in  4%  miles  or  at 
the  rate  of  about  56  feet  per  mile.  The  western  dip  from  the  crest  to 
Bport.,  sec.  36,  SE.,  No.  8,  is  321  feet  in  1%  miles  or  at  the  rate  of 
183  feet  per  mile.  The  dip  eastward  from  the  crest  to  Pet.,  sec.  29, 
NE.,  No.  7,  is  210  feet  in  seven-eighths  of  a  mile. 

The  two  lowest  points  along  the  western  flank  of  the  anticline  con- 
form to  the  440-foot  contour.  The  field  is  bounded  by  the  500-foot 
contour  on  the  west  and  the  600-foot  contour  on  the  east.  The  con- 
tours south  of  the  north  line  of  sections  5  and  6,  Bridgeport  township, 
were  broken  because  the  data  was  scattered  and  somewhat  indefinite. 


Kirkwood  Sand. 

The  Kirkwood  sand  was  first  developed  in  1907  by  the  Burton  Bros. 
Oil  Company  on  the  Thomas  Kirkwood  farm  in  the  E.  %  NE.  ^4  S€c- 
14,  Lawrence  township,  now  known  as  the  R.  M.  Kirkwood  farm  and 
operated  by  the  Bridgeport  Oil  Company.  This  sand  is  the  most  widely 
developed  and  productive  of  any  in  the  Lawrence  county  field.  It 
extends  from  section  36,  Petty  township,  to  section  8,  Dennison  town- 
ship and  spreads  into  all  outlying  pools,  thus  indicating  the  shape  and 
extent  of  the  Lawrence  county  field. 

The  Kirkwood  sand  is  the  most  widespread  sand  that  is  productive 
of  oil  in  the  Illinois  basin.  It  is  the  equivalent  of  the  Sparta  sand  of 
Randolph  county,  the  Lindley  gas  sand  of  Greenville,  the  Carlyle  oil 
sand  of  Clinton  county,  the  Benoist  sand  of  Marion  county,  and  the 
Oakland  City  sand  of  Pike  county,  Indiana.  This  sand  lies  low  in  the 
Chester  series  and  is  usually  overlain  by  a  succession  of  shales,  lime- 
stone, some  sandstone,  and  at  least  two  and  often  three  red  shales.  The 
second  red  shale  usually  serves  as  its  horizon  marker  as  the  red  rock 
is  easy  to  distinguish  because  it  discolors  the  water  used  in  drilling. 

The  Kirkwood  sand  is  lenticular  in  some  portions  of  the  field.  It  is 
subdivided  into  two  and  often  three  thin  lenses.  The  surface  of  the  top 
lens,  however,  is  uniform  over  the  county  and  is  taken  as  a  basis  of 
contouring. 

The  sand  shows  excellent  initial  productions  and  has  promise  of  being 
long  lived  and  steady  in  its  yield.  It  is  the  most  reliable  of  all  the 
sands.     There   is   little   or  no   gas   }deld   from   it   except  close  to   the 


110  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.      [bull.  no.  22 

northern  limits  of  the  county.  The  oil  is  a  "sweet"  oil  containing  a 
small  percentage  of  sulphur  and  has  about  30°  gravity,  Beaume. 

There  are  three  areas  in  the  field  where  this  sand  is  especially  pro- 
ductive. The  type  locality  includes  sections  11,  12,  14,  15,  Lawrence 
township  and  sections  22,  23,  25,  26  and  36,  Dennison  township.  The 
next  important  area  lies  about  the  anticlinal  dome  spoken  of  under 
the  discussion  of  the  upper  sand  beds  of  the  field,  page  107.  This 
area  includes  sections  19,  20,  29  and  30,  Petty  township,  and  sections  6, 
31,  32  and  36,  Bridgeport  township.  A  less  important  area  is  well 
developed  in  parts  of  sections  7,  8,  and  17,  Bridgeport  township. 

Data  from  220  wells  in  the  Lawrence  county  field  indicate  an  average 
interval  of  67  feet  between  the  Kirkwood  and  "Gas"  sands  in  the  upper 
part  of  the  field,  and  243  wells  indicate  an  average  interval  of  265  feet 
between  the  Kirkwood  and  Buchanan  sands  in  its  lower  part,  where  the 
"Gas"  sand  is  not  correlated.  The  average  interval  between  the  Kirk- 
wood and  "Gas"  sands  in  157  wells  in  Petty  township  is  63  feet.  There 
are  63  wells  in  the  northern  part  of  Bridgeport  township  that  show 
an  average  interval  of  78  feet  between  the  two  sands.  The  range  of 
interval  lies  between  26  and  134  feet. 

The  intervals  between  the  Kirkwood  and  Buchanan  sands  were  cal- 
culated for  that  portion  of  the  field  south  of  Petty  township.  Those  in 
Petty  township  were  not  averaged  because  of  the  uncertainty  of  corre- 
lation of  the  Buchanan  sand. 

There  are  85  wells  in  Bridgeport  township  that  show  an  average  in- 
terval of  255  feet  between  the  two  sands;  57  wells  in  Lawrence  town- 
ship with  an  interval  of  244  feet;  and  101  wells  in  Dennison  township 
with  an  average  interval  of  287  feet.  The  interval  therefore  seems  to 
increase  toward  the  southern  end  of  the  field.  There  are  eight  wells 
on  the  terrace  in  sections  20,  29  and  30,  Bridgeport  township  that  show 
an  average  interval  of  450  feet  between  the  sands.  This  seems  to 
indicate  a  rapid  thickening  of  the  formations  as  they  dip  west  into  the 
Illinois  basin,  adjacent  to  the  LaSalle  anticline.  The  wells  in  the 
eastern  extension  of  the  field  in  sections  11  and  12  of  Lawrence  town- 
ship indicate  a  lessening  of  interval  between  the  sands  and  an  average 
of  about  200  feet. 

The  thickness  of  the  Kirkwood  sand  is  very  irregular  over  the  field. 
It  is  found  to  average  about  30  feet  in  those  wells  that  pass  through 
the  sand. 


DETAILED   STRUCTURE, 

The  altitudes  of  the  top  lens  of  the  Kirkwood  sand  were  assembled 
and  contoured  in  Plate  IX.  The  contours  on  this  sand  give  a  most  com- 
plete and  satisfactory  idea  of  the  structure  of  the  LaSalle  fold.  The 
information  was  abundant  and  widely  distributed. 

The  upper  part  of  the  field  from  sections  35  and  36,  Petty  township, 
to  and  including  sections  7  and  8,  Bridgeport  township,  shows  an 
elongated  dome  or  double  plunging  anticline.  The  actual  top  of  the 
dome  lies  around  Pet.  sec.  30,  SE.,  No.  55.  The  sand  dips  in  four 
directions  from  this  well.     The  general  crest  lies  within  the  680-foot 


blatchley]  LAWREXCE    COUNTY    GEOLOGY.  Ill 

contour  and  has  an  areal  extent  of  about  80  acres.  A  part  of  it  overlaps 
into  section  29,  Petty  township.  The  sand  dips  240  feet  northward 
along  the  A- A  cross-section,  between  the  crest  and  Pet.  sec.  35,  IS'E., 
No.  2,  a  distance  of  5%  miles.  The  rate  of  dip  is  41  i'ect  per  mile. 
The  dip  to  the  east  along  the  C-C  cross-section  to  Pet.  sec.  20,  !SE., 
No.  10,  is  219  feet  in  iy8  miles  or  194  feet  per  mile.  The  dip  to  the 
west  along  the  same  cross-section  to  Bport.  sec.  36,  SE.,  No.  8,  is  342 
feet  in  iy2  miles  or  at  the  rate  of  228  feet  per  mile.  The  southward 
dip  of  the  sand  through  the  center  of  the  field  to  Den.  sec.  22,  NW., 
Nb.  5,  is  335  feet  in  b1/^  miles  or  at  the  rate  of  63  feet  per  mile. 

/The  dome-like  structure  merges  into  a  mild  trough  in  sections  4,  9, 
10,  Lawrence  township,  and  sections  21  and  22,  Dennison  township. 
The  sand  then  lies  flat  to  the  south  through  Lawrence  and  Dennison 
/townships  forming  a  broad  plateau-like  crest  of  the  major  fold.  The 
sand  lies  at  a  uniform  level  at  about  the  400-foot  contour.  The  sands 
on  both  sides  of  the  field  and  to  the  south  dip  toward  the  limbs  of  the 
major  fold.  The  southern  limits  of  the  field  seem  to  gradually  drop 
lower  than  the  producing  zone  of  the  sand.  Whether  the  major  fold 
continues  to  drop,  until  it  merges  into  the  southeastern  side  of  the 
eastern  interior  coal  basin  or  whether  the  drop  is  local,  as  seems  to  be 
the  case  between  Crawford  and  Lawrence  counties,  is  not  known.  At 
any  rate  the  anticline  loses  much  of  its  identity  as  a  structural  fold, 
thus  suggesting  its  mergence  into  the  rim  of  the  basin. 

The  terrace  in  sections  20,  29  and  30,  Bridgeport  township,  prev- 
iously spoken  of,  is  prominently  shown  by  the  Kirkwood  sand  contours. 
It  seemingly  covers  an  areal  extent  of  about  240  acres  and  lies  between 
the  100  and  120-foot  contours.  This  is  about  300  feet  lower  than  the 
producing  sand  in  the  Kirkwood  area  of  Dennison  township,  three  miles 
east.  Further  drilling  will  possibly  extend  production  until  the  area 
will  cover  several  times  its  present  extent. 

Tracey  Sand. 

The  Tracey  sand  was  first  developed  in  1908  by  Busch  and  Everett 
in  the  R.  J.  Tracey  farm  in  the  NW.  14,  NE.  y±,  sec.  13,  Lawrence 
township.  This  sand  is  not  found  widely  productive  of  oil.  The  type 
localities  lie  in  sections  11  and  14,  Lawrence  township;  sections  25  and 
26,  Dennison  township;  and  sections  19  and  30,  and  sections  25,  26, 
35  and  36,  Petty  township. 

This  sandstone  is  soft  and  calcerous.  It  overlies  the  Ste.  Genevieve 
and  massive  St.  Louis  limestones,  which  the  oil  men  often  call  the 
"big  lime."  The  Tracey  sand  lies  in  the  basal  portion  of  the  Tribune 
formation  and  does  not  correspond  to  the  Cypress  sandstone,  as  has 
been  suggested  by  the  author  in  his  earlier  studies  of  the  stratigraphy 
of  the  area.1 

Data  from  194  wells  over  the  entire  field  indicate  an  average  interval 
of  114  feet  between  the  Kirkwood  and  the  Tracey  sands.  The  average 
interval  for  each  of  the  townships  is  shown  in  the  following  table : 

1  Economic  Geology,  Vol.  VII,  No.  6,  September,  1912,  p.  579 


112  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.-    [bull.  no.  22 

Intervals  Between  Kirkwood  and  Tracey  Sands. 


Average 

interval 

Number 

between 

of 

the 

Township. 

wells  giving 

Kirkwood 

data. 

and  Tracy 

sands  in 

feet. 

Dennison . . . 

65 
21 

30 

78 

105 

Lawrence 

111 

Bridgeport 

118 

Petty 

120 

The  interval  seems  to  widen  as  the  sands  dip  into  the  limbs  of  the 
anticline.  The  interval  in  Pet.  sec.  15,  NE.,  No.  1,  is  160  feet  and  in 
Pet.  sec.  23,  NE.,  No.  1,  210  feet.  The  intervals  lessen  to  the  north 
to  about  40  feet.     This  fact  is  borne  out  by  the  A-A  cross-section. 

The  Tracey  sand  yields  excellent  pressures  of  gas  in  the  northern  half 
of  the  field.  The  gas  has  a  rank  odor  in  consequence  of  its  large  sulphur 
content,  and  the  oil  is  "sour."  This  sand  is  so  closely  associated  with 
the  underlying  limestones  that  its  oil  and  gas  probably  had  its  origin 
from  them. 

DETAILED  STRUCTURE. 

The  altitudes  of  the  top  of  the  Tracey  sand  were  assembled  and 
contoured  on  Plate  X.  The  data  were  too  scattered  to  warrant 
well  defined  contouring,  hence  many  of  the  contour  lines  are  broken 
to  indicate  merely  the  general  trend  of  the  structure.  Only  the 
type  localities  mentioned  above  justified  continuous  contour  lines.  The 
structure  of  the  sand  closely  resembles  that  of  the  overlying  Kirkwood 
except  that  the  dips  are  not  so  pronounced.  As  with  the  other  sands, 
the  Tracey  conforms  to  the  dome-like  structure  in  Petty  township.  The 
crest  of  the  dome  lies  at  Pet.  sec.  30,  SE.,  No.  63.  The  dip  northward 
to  Pet.  sec.  26,  NE.,  No.  2,  is  247  feet  in  6%  miles  or  at  the  rate  of 
37  feet  per  mile.  The  sand  appears  very  flat  in  parts  of  sections  12, 
13,  and  all  of  18,  about  l1/?  miles  north  of  the  apex  of  the  dome.  The 
fold  dips  equally  about  240  feet  to  both  sides  of  this  flat.  The  dip 
south  from  the  apex  of  the  dome  to  Law.  sec.  10,  SW.,  No.  1,  is  283 
feet  in  3%  miles  or  at  the  rate  of  73  feet  per  mile.  The  Tracey,  like 
the  Kirkwood  horizon,  assumes  a  plateau-like  nature  on  the  crest  of 
the  anticline  to  the  south  of  the  last  mentioned  well. 


McClosky  Sand. 


and  Gas 


%  section  25, 


The  McClosky  sand  was  developed  by  the  International  Oi 
Company  on  the  M.  McClosky  farm  in  the  NW.  %  SE. 
Dennison  township.  The  type  locality  for  this  sand  lies  in  sections  25 
and  36,  Dennison  township.  It  is  also  productive  at  the  same  level  in 
sections  11,  12,  13  and  14,  Lawrence  township.  This  formation  is 
extensively  developed  in  a  long  narrow  strip  beginning  in  the  NE.  *4 
section  6,  Bridgeport  township  and  extending  through  the  middle  of 
the  field  into  section  19,  Petty  township.  The  McClosky  sand  is 
widely  developed  in  the  northern  end  of  the  field  in  sections  1,  7,  11, 
12,  13,  18,  25,  35  and  36,  Petty  township. 


BLATCHLET] 


LAWRENCE    COUNTY    GEOLOGY. 


113 


The  McClosky  sand  is  a  soft  oolitic  limestone  known  as  the  Ste. 
Genevieve.  This  limestone  underlies  the  Cypress  and  Chester  rocks  and 
overlies  the  massive  and  hard  St.  Louis  limestone.  The  contact  between 
the  overlying  Chester  and  the  Ste.  Genevieve  in  Lawrence  county  is 
well  definedbut  the  lower  portion  of  the  Ste.  Genevieve  merges  into 
the  St,  Louis.  In  many  places  the  two  limestones  can  be  distinguished 
only  by  the  difference  in  their  hardness  and  the  presence  of  oolites  in 
the  Ste.  Genevieve. 

Data  from  150  wells  in  the  Lawrence  county  field  show  an  average 
interval  of  104  feet  between  the  McClosky  and  Tracey  sands.  The 
average  interval  in  each  of  the  townships  is  shown  in  the  following  table : 

Intervals  Between  Tracey  and  McClosky  Sands. 


Average 

intervals 

Number 

between 

of 

the  Tracey 

Township. 

wells  giving 

and 

data. 

McClosky 

sands  in 

feet. 

Dennison 

43 
14 
15 

113 

Lawrence 

118 

Bridgeport 

105 

Petty 

78 

96 

The  interval  widens  perceptibly  as  the  sand  clips  into  the  limbs  of  the 
anticline.  The  interval  in  Pet.  sec.  15,  NE.  No.  1,  is  174  feet  and  in 
Pet.  sec.  23,  NE.,  No.  1,  is  175  feet. 

The  McClosky  sand  has  yielded  the  largest  initial  productions  of  any 
of  the  producing  sands  in  Illinois.  It  is  not  widely  developed  because 
of  the  large  expense  incurred  in  drilling.  The  wells  in  the  northern 
section  of  the  field  have  been  good  producers  and  have  yielded  some 
gas.  The  oil  and  gas  have  a  large  sulphur  content.  The  southern  part 
of  the  field  has  yielded  several  oil  gushers  and  but  one  or  two  gas 
wells.  The  oil  has  a  much  smaller  sulphur  content  than  that  from  the 
northern  portion  of  the  field. 


DETAILED   STRUCTURE. 

The  altitudes  of  the  top  of  the  McClosky  sand  were  assembled  and 
contoured  in  Plate  XL  The  contours  reveal  one  major  and  three  minor 
domes  along  the  crest  of  the  anticline.  The  first  dome  lies  at  the 
northern  boundary  of  the  county,  in  sections  25  and  36,  Petty  township. 
It  falls  within  the  320-foot  contour.  The  top  of  the  dome  covers  about 
three-fourths  of  a  square  mile. 

The  sand  dips  from  this  dome  into  a  basin  about  90  feet  deep  and 
then  gradually  rises  into  a  terrace  through  sections  12,  13,  18  and  19, 
Petty  township.  The  terrace  merges  rapidly  into  the  major  dome  of 
the  fold  in  section  30,  Petty  township.  The  top  of  the  dome  lies  at 
Pet.  sec.  30,  SE.,  No.  59.  The  dip  from  the  apex  eastward  to  Pet. 
sec.  20,  SE.,  No.  10,  is  164  feet  in  1%  miles,  or  at  the  rate  of  145  feet 

—8  G 


114  OIL  FIELDS  OF  CRAWFOFiD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

per  mile.  The  dip  westward  to  Bport.  sec.  31,  SW.,  No.  5,  is  218  feet 
in  iy8  miles,  or  at  the  rate  of  193  feet  per  mile.  The  west  dip  of  the 
fold  is  45  feet  greater  than  the  east  dip  for  the  same  distance.  There 
are  two  very  small  domes  or  sharp  pinnacles  in  the  sand  immediately 
south  of  the  major  uplift.  The  crests  of  these  lie  at  Pet.  sec.  32,  SW., 
Nos.  10  and  17.  The  sand  lies  at  413  and  418  feet  respectively  above 
the  assumed  datum  plane  of  1,500  feet  below  sea  level  or  only  27  feet 
below  the  top  of  the  largest  dome. 

The  data  are  scanty  along  the  sides  of  the  main  anticline  and  there- 
fore the  contours  are  dashed.  They  show  strong  dips  to  both  sides  of 
the  field  and  a  long  gentle  dip  to  its  southern  end.  The  structure  of 
the  sands  in  the  southern  half  of  the  field  is  very  similar  to  that  of  the 
Kirkwood  and  Tracey  sands.  The  crest  of  the  anticline  merges  from 
the  major  dome  into  an  extensive  flat  area  which  lies  uniformly  around 
the  160-foot  contour. 

CROSS-SECTIONS. 

General  Statement. 

Four  cross-sections  were  constructed  along  lines  that  pass  through 
and  across  the  Lawrence  county  field.  They  were  chosen  especially  with 
respect  to  the  structure  of  the  area,  as  it  is  desired  to  show  the  nature 
of  the  crest  of  the  La  Salle  anticline  as  well  as  the  flanks.  The  sections 
were  also  chosen  along  lines  that  pass  through  or  near  a  large  number 
of  wells. 

The  cross-sections  were  constructed  by  plotting  records  with  respect 
to  sea  level.  A  line  representing  sea  level  was  drawn,  and  another  repre- 
senting an  ideal  surface  500  feet  above  it.  This  is  marked  off  to  corres- 
pond with  the  points  where  the  line  crosses  section  or  township  lines. 
The  names  of  the  townships  are  placed  in  their  proper  positions.  The 
records  of  the  wells  were  located  with  respect  to  their  position  along  the 
line  and  above  sea  level.  They  were  then  plotted  with  uniform  symbols 
and  scale.  Wherever  the  cross-section  line  cut  a  contour- line  the  alti- 
tude of  the  contour  was  marked  with  a  cross  and  set  in  its  proper 
position.  Correlation  lines  were  then  drawn  through  all  crosses  repre- 
senting the  altitude  of  a  particular  sand  and  between  similar  formations 
in  detailed  records.  Since  a  datum  plane  1,500  feet  below  sea  level  was 
used  to  make  the  contouring  read  positive  this  line  is  drawn  on  the 
sections  merely  to  emphasize  its  use.  The  position  of  any  sand  can  be 
measured  directly  above  the  datum  plane  line  and  the  figures  thus  ob- 
tained should  correspond  with  those  obtained  from  the  structure  maps 
and  those  recorded  in  the  tables  of  well  data. 

Cross-section  A-A. 

The  A-A  cross-section,  PL  XII,  presents  the  structure  of  the  sands 
along  the  crest  of  the  anticline  and  through  the  middle  of  the  entire 
Lawrence  county  field.  As  a  whole  the  section  is  especially  valuable 
since  it  shows  the  double  plunging  anticline,  the  crest  of  which  lies  in 
section  30,  Petty  township,  the  convergence  of  the  sands  at  the  northern 
end,  and  the  dip  from  the  dome  into  the  flat  at  the  southern  end  of  the 


BLATCHLEY] 


LAWRENCE    COUNT!    CROSS-SECTIONS. 


115 


field.  The  sands  are  shown  to  be  generally  parallel  with  local  irregu- 
larities that  seem  due,  in  most  cases,  to  the  thinning  and  thickening  of 
the  sand.  All  sands  conform  to  a  mild  basin  at  the  foot  of  the  elongated 
dome  in  sections  9  and  16,  Lawrence  township. 


LOGS. 

The  section  is  made  up  from  many  skeleton  logs  which  are  found  in 
the  tables  of  well  data.     The  detailed  logs  are  presented  below. 
The  records  of  the  following  wells  are  found  in  the  tables : 


List  of  Wells  in  Lawrence  County  Furnishing  Data  for  Cross-Section  A-A. 


Township. 

Section. 

Quarter- 
section. 

Well 
number. 

Petty..                  

26 

NE. 
SE. 
NE. 
NW. 

sw. 
sw. 

NE. 

NE. 

NE. 

NE. 

NE. 

SE. 

SE. 

NW. 

NW. 

NW. 

SW. 

sw. 

NW. 
NW. 
NW. 
NW. 

SW. 

SE. 

SE. 

SE. 

SE. 

NE 

NE. 

NE. 

SE. 

SE. 

SE. 

SE. 

NW. 

NW. 

SW. 

SW. 

NW. 

NW. 

NE. 

NE. 

SE. 

SW. 

NE. 

NW. 

NW. 

NW. 

SW. 

sw. 

SE. 
NE. 

NE. 
SW. 
SW. 
NW. 

NE. 

NE. 
SE. 

1 

26 

4 

35 

2 

36 

11 

36 

5 

36 

6 

12 

4 

12 

12 

6 
14 

12 

12 

12 

12 

10 

12 

9 

18 

17 

18 

16 

18 

15 
1 

18 

18 

3 

19 

3 

19 

19 

5 

19 

g 

19 

21 

19 

19 

19 

16 

19 

14 

19 1 

3 

30 

13 

30 

15 

30 .' 

26 

30 

60 

30 

59 

30 " 

69 

30     

76 

Bridgeport 

32 

35 

32 

33    34 

32 

'   23 

26 

9     10 

5 

4 

10 

9 

5 

15 

Lawrence 

9 

15 

9 

4 

12 

15 

11 

7 

15 

22 

20 

15 

1 

Dennison 

4 

22 

8 

23 

1 

23 

26 

1 

26 

14 

10 

26 

15 

116  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

List  of  Wells  in  Lawrence  County — Concluded. 


Township. 

Section. 

Quarter- 
section. 

Well 
number. 

Dennison—  Concluded . . 

25 

SW. 

sw. 

NW. 

NE. 

SE. 

SE. 

SE. 

NW. 

NW. 

SE. 

NW. 

NW. 

2 

25 

3 

36 

2 

36 

1-3 

36 

19 

36 

16 

36 

9 

6 

5 

6 

4 

6    

1 

8 

1 

8 

2 

The  following  logs  are  those  shown  in  detail  in  the  cross-section  and 
briefly  referred  to  in  the  tables: 

Pet:  sec.  36,  SW.,  No.  8. 

Operator — Snowden  Bros. 
Farm  and  well — Petty,  No.  1. 
Elevation— 436  feet. 


Sand  and  gravel,  loose   

Slate,    blue,    soft    

Limestone,  gray,  hard   (3  bailers  water,  190  feet) 

Slate,   brown,   soft    

Limestone,    yellow,    hard    

Slate,    blue     

Slate,    brown,   hard    

Slate,  black,  soft    

Coal     

Shells     

Slate,  white,   hard    

Shell,   blue,    hard    

Coal   

Slate,    blue,    soft    

Shale,  white,  hard    

Shale,    brown,    soft    

Slate,  black,  soft   

Slate,   blue,   soft    

Slate,    brown,    hard    

Limestone,   white,   hard    

Shale,    white,    soft    . 

Limestone,    blue,    hard    

Shells,    hard 

Limestone,   red,   soft 

Slate,   blue,   soft    

Limestone,  blue,  hard  (2  bailers  water,  800  feet). 

Slate,    blue,    soft 

Limestone  shells,  gray,  hard 

Slate,     black 

Sand,  white   (10  bailers  water  per  hour,  885  feet) 

Slate  and  shells,  blue 

Sand  (hole  full  of  water,  980  feet) 

Slate,    blue,    soft 

Sandy   shale,    brown 

Sand,    white,    soft 

Slate,    black 

Sand,  gray,  hard 

Slate,    black 

Sand,    white 

Slate,  brown,  soft 

Sand,    loose 

Slate,  light  brown,  soft 

Limestone,     hard 

Sand,  white,   hard 

Limestone,   gray,  hard 

Slate,    blue,    soft 

Sandy    limestone 

Oil    sand 


Thickness 

Depth 

Feet 

Feet 

112 

112 

68 

180 

10 

190 

110 

300 

6 

306 

10 

316 

124 

440 

10 

450 

4 

454 

15 

469 

55 

524 

5 

529 

5 

534 

56 

590 

15 

605 

85 

690 

10 

700 

10 

710 

15 

725 

10 

735 

10 

745 

20 

765 

15 

780 

5 

785 

10 

795 

5 

800 

15 

815 

20 

93  S 

35 

870 

15 

885 

35 

920 

60 

980 

25 

1,005 

90 

1,095 

8 

1,103 

10 

1,113 

62 

1,175 

10 

1,185 

35 

1,220 

20 

1,240 

15 

1,255 

5 

1,260 

5 

1,265 

10 

1,275 

1,285 

13 

1,298 

28 

1,326 

10 

1,336 

BLATCHLEY] 


LAWRENCE    COUNTY    CROSS-SECTIONS. 


117 


Logs — Continued. 


Thickness  Depth 

Feet  Feet 

Slate,    blue,    soft 10  1,346 

Limestone,    yellow,    hard 20  1,366 

Oil  sand,   white,   soft •       26  1,392 

Limestone,  gray 8  1,400 

Sand,  white,   oil 12  1,412 

Slate,  blue,  soft .10  1,422 

Total    depth 1,422 

Initial   production,    125    bbls. 

Pet.  Sec.  36,  SW.,  No.  10. 


Operator — Snowden  Bros. 
Farm  and  well — Petty,  No.  3. 
Elevation— 435  feet. 


Sand,  white,  soft 

Slate,  blue,  soft 

Limestone,   light,  hard 

Sand,  white,  hard 

Slate,  blue,  soft 

Limestone,   gray,   hard 

Sand,  white,  hard 

Slate,  white,  soft 

Limestone,   light,   hard 

Slate,  white,  soft 

Limestone,   light,   hard 

Slate,  light  brown,  soft 

Sand,  hard   (oil  1,328  to   1,332  feet) 

Slate,  light  brown 

Limestone,  gray,   hard 

Slate,  blue,  soft 

Sand,  white,  soft  (oil  1,3-75  to  1,387  feet) 

Slate,   blue,  hard 

Limestone,     hard 

Sand,  white,  soft 

Limestone,    blue,   hard 

Total  depth 


Thickness 

Depth 

Feet 

Feet 

100 

970 

130 

1,100 

15 

1,115 

100 

1,215 

10 

1,225 

5 

1,230 

15 

1,245 

5 

1,250 

30 

1,280 

5 

1,285 

20 

1,305 

5 

1,310 

22 

1,332 

15 

1,347 

17 

1,364 

3 

■1,367 

20 

1,387 

5 

1,392 

10 

1,402 

12 

1,414 

21 

1,435 

1,435 

Pet.  sec.  1,  NW.,  No.  3. 


Operators — Snowden  Bros. 
Farm  and  well — Drole,  No.  7. 
Elevation — 435  feet. 


Thickness  Depth 

Feet  Feet 

Clay,    soft 18  18 

Sand  and  gravel,   soft 96  114 

Slate,    soft 108  232 

Sand,    hard 10  242 

Shell,   hard    (water) 23  265 

Slate,  white,  hard 95  360 

Slate,  dark,  hard 60  420 

Shell,    hard 5  425 

Coal     6  431 

Slate,    light,    soft 269  700 

Shell,   light,  hard 25  725 

Slate,  light,  dark,  red  and  blue,  soft 90  815 

Sand,   hard    (water) 25  840 

Slate,    light,    soft 10  850 

Sand,  white,  loose 45  895 

Slate,    light,    soft 5  900 

Sand,   white,   hard 63  963 

Slate,    light,    soft 50  1,013 

Slate,  dark,  hard 40  1,053 

Limestone,  gray,  hard 7  1,060 

Slate,    light,    soft 50  1,110 

Sand,  gray,  loose   (water,   1,150  to  1,240  feet) 40  1,150 

Sand,  white,   hard 90  1,240 

Limestone,  gray,  hard 30  1,270 


118 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES',    [bull.  no.  22 


Logs — Continued. 


Slate,    dark 

Slate,  light,  loose.... 
Oil   sand,   gray,   loose. 

Slate,  dark,  hard 

Limestone,  gray,  hard 
Sand,  white,  loose.  .  . 
Slate,  black,  hard.... 
Sand,   white,   hard.... 

Oil  sand 

Slate,  dark,  hard.  .  .  . 
Limestone,  gray,   hard 

Total  depth 


Thickness 

Depth 

Feet 

Feet 

20 

1,290 

28 

1,318 

8 

1,326 

12  . 

1,338 

25 

1,363 

12 

1,375 

9 

1,384 

18 

1,402 

10 

1,412 

2 

1,414 

17 

1,431 

1,431 

Pet.  sec.  1,  SW.,  No.  5. 


Operators — Snowden  Bros. 
Farm  and  well — Piper,  No.  9. 
Elevation— 435  feet. 


Soil    

Mud,    blue,    soft 

Slate,    light,    soft 

Sand,   white,   soft    (water)  .  .  . 

Slate,    light,    soft 

Coal     

Slate,    light,    soft 

Limestone,  white,  soft 

Slate,  white,  soft 

Slate,    black 

Slate,    white 

Limestone,   white,    hard 

Slate,  white,  soft 

Slate,    black 

Slate,    light 

Coal    

Limestone,   white,   hard 

Slate,  black,   soft 

Sand,  white,  soft 

Coal     

Slate,    white 

Slate,   brown 

Slate,    white 

Sand,  white,  hard 

Slate,  white,  soft 

Slate,   brown 

Slate,    black 

Slate,    light 

Limestone,   white,   hard 

Sand,  white,   hard 

Slate,    white,    loose 

Slate,   brown,  loose 

Limestone,   white,   hard 

Slate,  white,  soft 

Slate,    black 

Limestone    shell,    hard 

Sand,    brown,    open 

Shale    

Sand,    white 

Limestone,,  gray 

Sand,    white 

Slate,  black 

Limestone  shell,  hard 

Slate     

Sand,  white,  soft 

Limestone  shell,  hard 

Red    rock 

Slate,   black 

Limestone,    white,    hard 

Slate,    black 

Sand,   gray .  .  . 

Slate,    black 

Total  depth 

Initial  production,   90  bbls. 


Thickness 

Depth 

Feet 

Feet 

18 

18 

4 

22 

34 

56 

2 

58 

57 

115 

2 

117 

123 

240 

6. 

246 

59 

305 

20 

325 

30 

355 

8 

363 

15 

378 

32 

410 

10 

420 

3 

423 

3 

426 

42 

468 

7 

475 

4 

479 

21 

500 

52 

552 

20 

572 

6 

578 

17 

595 

45 

640 

12 

652 

33 

685 

5 

690 

10 

700 

10 

710 

40 

750 

10 

760 

g 

765 

30 

795 

10 

805 

11 

816 

824 

15 

839 

12 

851 

122 

973 

1,014 

5 

1,019 

120 

1,139 

68 

1,207 

28 

1,235 

10 

1,245 

1,252 

23 

1,275 

25 

1,300 

12 

1,312 

1,326 

1,326 

BLATCHLEY] 


LAWRENCE    COUNTY    CROSS-SECTIONS. 


119 


Logs — Continued. 
Pet.  sec.  30,  NE.,  No.  9. 


Operators — Bridgeport  Oil  Company. 
Farm  and  well — Boyd,  No.  11. 
Elevation — 452  feet. 


Mud  and  slate 

Limestone    

Slate    

Sand    

Slate    

Limestone 

Slate     

Sand    -. 

Slate    

Limestone,   hard 

Slate    

Sand    

Slate    

Coal    

Slate    

Limestone    shell 

Coal    

Slate    

Sand    

Coal     

Shale,    brown 

Sand    

Slate     

Limestone     shell 

Sand     

Slate     * 

Limestone     shell 

Slate     

Limestone     shell 

Slate     

Stray    sand 

Slate    

Sand     

Sand,   broken 

Oil  sand    (best  oil,   933   to   950   feet). 

Total     depth 


Thickness 

Depth 

Feet 

Feet 

44 

44 

6 

50 

20 

70 

20 

90 

55 

145 

15 

160 

5 

165 

25 

190 

10 

200 

5 

205 

45 

250 

40 

290 

50 

340 

5 

345 

55 

400 

10 

410 

5 

415 

100 

515 

5 

520 

3 

523 

32 

555 

30 

585 

15 

600 

608 

64 

672 

700 

5 

705 

780 

5 

785 

830 

13 

843 

876 

4 

880 

15 

895 

57 

952 

952 

Pet.  sec.  30,  SE.,  No.  50. 


Operators — Curtis  and  Akin. 
Farm  and  well — Fitch,  No.  17. 
Elevation — 475  feet. 


First  water  at 

Red  rock  at 

Sand    at 

Bottom    of    sand 

Slate     

Limestone    shells 

Sand  (show  of  oil,  773  feet) 

Slate     

Sand    (oil,    945    feet) 

Slate    

Sand    

Sand   and    limestone 

Red   rock 

Slate     

Limestone    

Slate     

Sand    (gas) 

Limestone     

Slate     

Red   rock 

Sand    (oil,    1,340   feet) 

Slate     


Thickness  Depth 

Feet  Feet 

120 

217 

612 

78  690 

34  724 

4  728 

124  852 

53  905 

90  995 

65  1,060 

45  1,105 

20  1,125 

1,159  to  1,166 

4  1,170 

20  1,190 

34  1,224 

4  1,228 

16  1,244 

41  1,285 

15  1,300 

40  1,340 

28  1,368 


120  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

Logs — Continued. 


Thickness     Depth 
Feet  Feet 

20         1,388 
10         1,398 
1,424 


Sand     

Slate     '.'.'.'.'.'.'.'.'.'.'.'.'.'.  '..".  '.'.'.'.'..'".'. 

Sand   (little  oil,  best  showing,  1,411  feet).  ...  ..'.'....'.'.'...'.'.'.'.'.'.'.  26 

Total    depth 777777        1,424 

Bport.  sec.  32,  NW.,  No.  23. 

Operators — Snowden  Bros. 
Farm  and  well — Perkins,  No.  28. 
Elevation— 511  feet. 


Clay    

Slate    '.".'. 

Sand    

Slate    

Shell    

Slate    ..'.'..'.'.'.'.'. 

Slate    and    shells 

Slate    ...'.'.'.'.'.'.'. 

Limestone    

Slate '.'.'.'.'.'.'.'.'. 

Limestone    

Slate    .....! 

Limestone    shells 

Slate 

Limestone    shells 

Slate    i  .  . 

Sand    

Slate    v .' 

Limestone     

Slate    

Slate    and    shells 

Sand  and  limestone    (oil,   890  feet) 

Sand    

Slate    

Limestone     

Sand    

Shells    

Sand    

Slate    

Limestone    

Slate    

Limestone    

Slate    

Limestone    

Slate    

Red   rock 

Slate    

Shells    

Limestone     

Slate    

Limestone   (little  gas,  1,290  feet) 

Slate    

Gas  sand    (gas,   1,322   feet) 

Slate    

Red    rock 

Slate    

Oil  sand   (oil,  1,370  to  1,384  feet) 

Slate    

Sand    

Slate    

Oil  sand   (oil,   1,468  to  1,482  feet) 

Slate 

Limestone    

Total    depth 

Bport.  sec.  32,  NW.,  No.  19. 

Operators — Snowden  Bros. 
Farm  and  well— Perkins,  No.  22. 
Elevation — 488  feet. 


Thickness 

Depth 

Feet 

Feet 

20 

20 

80 

100 

60 

160 

109 

269 

6 

275 

75 

350 

50 

400 

100 

500 

8 

508 

72 

580 

4 

584 

132 

716 

4 

720 

45 

765 

6 

771 

23 

794 

26 

820 

17 

837 

10 

847 

8 

855 

30 

885 

5 

890 

25 

915 

60 

975 

17 

992 

21 

1,013 

11 

1,024 

66 

1,090 

1,096 

29 

1,125 

1,140 

16 

1,156 

1,163 

14 

1,177 

1,210 

6 

1,216 

1,236 

24 

1,260 

1,264 

19 

1,283 

1,315 

6 

1,321 

1,330 

15 

1,345 

1,351 

15 

1,364 

1,386 

12 

1,400 

1,412 

50 

1,462 

1,490 

7 

1,497 

8 

1,505 

1,505 

BLATCHLEY] 


LAWKENCE    COUNTY    CEOSS-SECTIONS. 


121 


Logs — Continued. 


Clay     

Slate    

Sand   (water,   135   to  150  feet) 

Slate    •• 

Sand    

Slate    

Limestone    shells 

Slate,    red 

Slate    

Sand    

Slate,    dark 

Slate,    light 

Slate,    dark 

Sand   shells 

Slate,    dark 

Slate,    light 

Limestone    shells 

Slate    

Slate  and  shells,   light 

Slate  and  shells,  dark 

Sand    

Slate    

Sand    

Slate    

Sandy   limestone 

Sand    

Total  depth 


Thickness 

Depth 

Feet 

Feet 

23 

23 

52 

75 

75 

150 

25 

175 

70 

245 

4 

249 

6 

255 

5 

260 

125 

385 

10 

395 

30 

425 

40 

465 

20 

485 

5 

490 

670 

23 

693 

705 

25 

730 

55 

785 

43 

828 

850 

20 

870 

30 

900 

45 

945 

985 

28 

1,013 

1,013 


Bport.  sec.  32,  SW.,  No.  5. 


Operators — Snowden  Bros. 
Farm  and  well — Perkins,  No.  17. 
Elevation— 479  feet. 


Clay    

Slate    

Sand    

Slate    

Sand    

Limestone    

Slate    

Red   rock 

Slate    

Sandy   limestone 

Slate 

Limestone    

Slate     

Limestone    

Coal     

Limestone 

Slate    

Sandy  shells 

Slate     

Sandy   shells 

Sand    

Slate    

Sand    

Slate    and    shells 

Sand    

Slate    and    shells 

Limestone    

Sand    

Slate    

Sand    

Slate    

Sand  and  slate 

Slate    

Sand   (oil,   925  to  935  feet) 

Slate    

Limestone,    gritty 

Sand   (oil,  1,045  feet;  water,  1,050  feet) 

Slate    

Sand    


jckness 

Depth 

Feet 

Feet 

20 

20 

60 

80 

70 

150 

15 

165 

89 

254 

6 

260 

5 

265 

5 

270 

175 

445 

10 

455 

20 

475 

5 

480 

10 

490 

3 

493 

3 

496 

7 

503 

87 

590 

5 

595 

95 

690 

10 

700 

10 

710 

32 

742 

6 

748 

37 

785 

15 

800 

45 

845 

5 

850 

7 

857 

18 

875 

15 

890 

14 

904 

6 

910 

10 

920 

42 

962 

13 

975 

45 

1,020 

85 

1,105 

3 

1,108 

28 

1,136 

122 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no. 


Logs — Concluded. 


Slate    

Sand    

Slate    

Limestone    

Red  slate 

Slate    and    shells 

Limestone. 

Slate  and  shells 

Red  slate 

Sand    (gas,    1,267   feet) 

Limestone    

Red    slate 

Slate    

Sand    (oil,    1,351   feet) 

Slate    

Sand  and  shells 

Slate    and    shells 

Sand    (oil,    1,461    feet) ' 

Slate    

Sand    (gas,    1,490   feet) 

Slate  and  shells 

Limestone    and    slate 

Sand    (gas,    1,580   feet) 

Limestone,    gritty 

Limestone  and  sand   (show  of  oil,   1,695  feet) 
Sandy   limestone 

Total    depth 


Thickness 

Depth 

Feet 

Feet 

2 

1,138 

22 

1,160 

24 

1,184 

3 

1,187 

6 

1,193 

27 

1,220 

25 

1,245 

13 

1,258 

4 

1,262 

28 

1,290 

15 

1,305 

25 

1,330 

20 

1,350 

1,395 

21 

1,416 

14 

1,430 

20 

1,450 

1,460 

15 

1,475 

1,500 

40 

1,540 

30 

1,570 

25 

1,595 

45 

1,640 

55 

1,690 

1,714 

1,714 


Bport.  sec.  32,  SW.t  No.  13. 


Operators — Snowden  Bros. 
Farm  and  well — Perkins,  No.  16. 
Elevation — 494  feet. 


Thickness        Depth 
Feet  Feet 

Sand    (water) 130  125  to 

Limestone  shell,  very  hard 10  270  to 

Red    rock 7  285  to 

Coal    6  430   to 

Coal     *• 5  500   to 

Limestone    shell 7  710   to 

Sand     5  720   to 

Sand    (show  of  oil,   805   feet) 26  800   to 

Oil   sand    (water,    880    feet) 75    -       840  to 

Sand,   hole  full  of  water 96        1,060  to 

Slate  and  shells 9        1,156  to 

Limestone     15 

Slate    3£ 

Red    slate 5 

Slate 20 

Limestone     ° 

Slate    J 

Limestone    11 

Slate    14 

Red    slate 

Slate    2 

Sand    (gas,    1,285   feet) 20 

Slate     : \ 

Limestone     ° 

Slate    33, 

Red  slate ° 

Slate  

Sand    (oil', '  1,378'  and  '  1,398    feet) 54 

Slate  3" 

Sand   (pay,"  '£,445"  to"  1,450  feet) 17 

Slate     19 

Sand    14 

Slate     IJ 

Limestone    5 

Total   depth v 

Production,   100  bbls. 


255 
280 
292 
436 
505 
717 
725 
826 
915 
150 
165 
180 
210 
215 
235 
243 
247 
258 
272 
278 
280 
300 
305 
311 
344 
350 
356 
410 
443 
460 
479 
493 
503 
508 


1.51  N 


BLATCHLEY] 


LAWRENCE    COUNTY    CROSS-SECTIONS. 


123 


Cross-section  B-B. 

The  B-B  crsos-section,  PL  XIII,  shows  the  structure  of  the  northern 
end  of  the  field.  .  It  crosses  the  field  diagonally  between  Pet.  sec.  15, 
NE.,  No.  1,  and  Pet.  sec.  30,  SW.,  No.  1.  The  sands  above  the  "Gas" 
sand  were  not  correlated  because  of  their  irregularity.  The  lower  sands 
show  the  major  arch  of  this  region  to  be  about  250  feet  high  and  three 
miles  wide.     The  section  is  made  up  of  the  following  records. 

LOGS. 

The  records  of  the  following  wells  are  found  in  the  tables  of  well 
data: 

List  of  Wells  in  Lawrence  County  Furnishing  Data  for  Cross-Section  B-B. 


Township. 

Section. 

Quarter- 
section. 

Well 
number. 

Petty.. 

2 

SE. 
SE. 
SE. 
NE. 
SW. 
SW. 
NE. 
NE. 
SW. 

2 

2 

7 

2 

2 

6 

36 

13 

36 

1 

36 

7 

36 

6 

30 

1 

Pet.  sec.  15?  NE.,  No.  1. 
Presented  in  the  stratigraphic  discussion,  page  80. 


Pet.  sec.  2,  SW..  No.  6. 

Operators — Snowden  Bros. 

Farm  and  well — Armitage,  No.  2. 

Elevation — 445  feet. 

Thickness     Depth 

Feet  Feet 

Soil,    yellow 33  33 

Slate,    dark 162  195 

Sand,    light 15  210 

Slate,    dark 35  245 

Limestone,     light 8  253 

Slate,  white,  soft 25  278 

Limestone,   white 15  293 

Slate,  white,  soft 17  310 

Sand,   light    (7  bailers  of  water  per  hour,    345   feet) 35  345 

Slate  and  limestone  shells,  light,  hard 11  356 

Red    rock 9  365 

Slate,  white 20  385 

Sand,    white 20  405 

Slate,    black,    soft 75  480 

Sand,     light 15  495 

Slate,     light 25  520 

Limestone,    light 15  535 

Slate    and    shells 30  565 

Limestone,   light,   hard 12  577 

Slate,    black,    soft 13  590 

Limestone,   white,   medium 15  605 

Slate,    dark,    soft 55  660 

Sand,     light 40  700 

Slate,    light,    soft 100  800 

Limestone,   light,   hard 7  807 

Slate,    dark,    soft 12  819 


124 


OIL  FIELDS  OF  CKAWFOED  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


Logs — Continued. 


Red    rock 

Limestone,   white,   hard 

Sand,    white 

Slate,   dark,    soft 

Limestone,    white,   hard 

Sand,    white    , 

Slate,    dark,    soft 

Sand,     white 

Sandy  limestone,  white 

Slate  and  shells 

Sand    (hole  full  of  water,   1,140   feet) 

Slate,    black 

Limestone    shells    and   sand 

Slate,    dark,    soft 

Limestone    shells,    light 

Slate    and    shells,    light 

Sandy   limestone 

Slate    and    shells 

Limestone,   light,   hard 

Slate  and  shells 

Limestone,   light,   hard 

Slate    

Limestone,    light,    hard 

Slate,    white,    soft 

Red   rock 

Sand,  light    (show  of  oil,   1,505   feet) 

Slate    and    shells 

Sand    (oil,   1,555   feet) 

Slate 

Limestone  and  sand   (oil,   1,578  to  1,583  feet) 
Slate     

Total  depth 


Thickness* 

Depth 

Feet 

Feet 

10 

829 

15 

844 

25 

869 

40 

909 

15 

924 

12 

936 

15 

951 

13 

964 

30 

994 

146 

1,140 

30 

1,170 

5 

1,175 

20 

1,195 

45 

1,240 

1,243 

42 

1,285 

1,300 

15 

1,315 

1,320 

115 

1,435 

1,440 

18 

1,458 

1,480 

15 

1,495 

1,505 

6 

1,511 

1,535 

30 

1,565 

1,577 

20 

1,597 

13 

1,610 

1,610 


Pet.  sec.  2,  SE.,  No.  10. 
Presented  in  the  stratigraphic  discussion,  page  81.  / 

Pet.  sec.  1,  NW.,  No.  3. 
Presented  in  the  discussion  of  the  A-A  cross-section,  page  117. 

Pet.  sec.  36,  SW.,  No.  10. 
Presented  in  the  discussion  of  the  A-A  cross-section,  page  117. 

Pet.  sec.  36,  NE.,  No.  10. 

Operators — Snowden  Bros. 
Farm  and  well — Nutall,  No.  5. 
Elevation— 435  feet. 

Thickness  Depth 

Feet  Feet 

Gravel,    yellow,    soft 180  180 

Slate,  black,  soft 80  260 

Limestone,    white,    hard    (water) 40  300 

Sand,  white,  hard   (12  bailers  water,   305   feet) 5  305 

Red   rock 5  310 

Slate,    white,    soft 60  370 

Limestone,  white,  hard 85  455 

Sand,   white,   soft    (water) 45  500 

Slate,    white,    soft 40  540 

Slate,    black,    soft 25  565 

Slate   and  limestone  shells 70  635 

Slate,    black,    soft 90  720 

Sand,   white,   soft    (water) 25  750 

Slate,    white 35  785 

Sand   (hole  full  of  water,   1,000  feet) 215  1,000 

Limestone,   white,   hard 95  1,095 

Sand,    white,    hard , 65  1,160 


124  oi 


Red    rock. . . . 
Limestone,   w 
Sand,    white . 
Slate,    dark, 
Limestone,   w 
Sand,    white 
Slate,    dark, 
Sand,     white 
Sandy  limesl 
Slate  and  sh 
Sand    (hole 
Slate,    black. 
Ljmestone    s 
Slate,    dark, 
Limestone    s 
Slate    and    s 
Sandy   limes 
Slate    and    s 
Limestone,   1 
Slate  and  si 
Limestone,   1 

Slate    

Limestone, 
Slate,    white 
Red   rock . . 
Sand,  light 
Slate    and    ! 
Sand    (oil, 

Slate    

Limestone  ; 
Slate     

Total  6 


Present* 


Present* 


Present 


Operate 
Farm  a 
Blevati 


Gravel,  y> 
Slate,  bla- 
Limestone 
Sand,  wh 
Red  rock 
Slate,  wh 
Limestone 
Sand,  wh 
Slate,  wl 
Slate,  bis 
Slate  anc 
Slate,  bl; 
Sand,  wh 
Slate,  wl 
Sand  (he 
Limeston 
Sand,    w 


BLATCHLET] 


LAWRENCE    COUNTY    CROSS-SECTIONS. 


125 


Logs — Concluded. 


Sand,    slate,    and   shells,    dark 

Slate,  white,   hard 

Sand,    white,    hard 

Limestone,   white,   hard 

Red   rock 

Limestone,   white,   hard 

Slate,    black,    soft 

Oil   sand,   gray 

Slate,  black 

Sand,  white    (4  bailers  of  water,   1,465  feet).... 

Slate    

Limestone,    white,    soft 

Limestone,   yellow,   hard    (oil,    1,564   feet) 

Sandy  limestone,   white,   soft 

Sand,  green  oil,  hard    (first  showing,    1,612   feet) 
Slate,    black,    soft 

Total    depth 


Thickness 

Depth 

Feet 

Feet 

50 

1,210 

50 

1,260 

35 

1,295 

15 

1,310 

5 

1,315 

100 

1,415 

19 

1,435 

9 

1,444 

11 

1,455 

10 

1,465 

25 

1,490 

60 

1,550 

15 

1,565 

4 

1,569 

1,622 

15 

1,637 

1,637 

Cross-section  C-C. 

The  C-C  cross-section,  PI.  XIV,  is  chosen  along  a  line  crossing  the 
crest  of  the  large  dome  in  section  30,  Petty  township.  This  cross-sec- 
tion presents  the  extreme  structure  of  the  Lawrence  county  field.  It 
shows  the  arch  to  he  about  400  feet  high  and  three  miles  wide.  Corre- 
lation lines  of  five  sands  are  drawn  over  the  dome  and  reveal  some 
irregularities  of  interval,  particularly  between  the  Kirkwood  and  Tracey 
sands  and  the  Buchanan  and  "Gas"  sands. 

The  section  is  made  up  of  the  following  records: 

LOGS. 

The  records  of  the  following  wells  are  in  the  tables  of  well  data : 
List  of  Wells  Affording  Data  for  Cross-Section  C-C. 


Township. 

Section. 

Quarter- 
section. 

Well 
number. 

36 

NE. 
NW. 
NW. 
SW. 

sw. 

SE. 
SE. 

SE. 

SE. 

SE. 

SE. 

NW. 

NW. 

NW. 

SE. 

7 

31 

5 

31 

4 

Petty 

30 

13 

30 

12 

30 

18 

30 

15 

30 

64 

30 

63 

30 

52 

30 

53 

29 

30,   31 

29 

29 

29 

2 

20 

3 

The  remaining  detailed  logs  of  the  section  are  presented  as  follows : 


Bport.  sec.  36,  SE.,  No.  8. 


Operators — Bridgeport  Oil  Company. 
Farm  and  well — Stoltz,  No.  13. 
Elevation — 523  feet. 


126 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.       [bull.  no.  22 


Logs — Continued. 

Thickness 
Feet 

Slate    and    shells 65 

Limestone    20 

Slate     25 

Limestone    10 

Sand    15 

Slate    105 

Sand    (water) 40 

Sand    20 

Slate    40 

Coal     5 

Limestone    35 

Big    limestone    shell 40 

Red   rock 8 

Slate    13 

Limestone    (  ?)    (probably  slate  and  shells) 139 

Slate    20 

Limestone   (  ?)    (probably  slate  and  shells) 170 

Sand    ( salt   water) 25 

Black   slate 55 

Sand    40 

Sand    (water) 45 

Slate    12 

Coal    2 

Slate    10 

Limestone     5 

Slate     3 

Sand    .  . 8 

Slate    45 

Sand     15 

Slate    20 

Limestone    3 

Slate    40 

Limestone    2 

Slate    25 

Limestone    21 

Salt    sand 99 

Slate    15 

Sand    (salt   water) 60 

Slate     27 

Limestone    37 

Slate    20 

Sand    10 

Slate     15 

Limestone     20 

Slate    10 

Sand  (water) 20 

Slate 8 

Limestone     5 

Slate     17 

Limestone     10 

Slate     17 

Red    rock 13 

Slate    5 

Limestone    35 

Slate     20 

Sand    ( 5  bailers  of  water  per  hour) 10 

Limestone    25 

Slate     : 43 

Limestone     2 

Slate    4 

Sand    (oil,    1,689    feet) 21 

Sand,    broken 10 

Slate     5 

Sand,    broken 12 

Slate    6 

Total     depth 


Depth 

Feet 

65 

85 

110 

120 

135 

240 

280 

300 

340 

345 

380 

420 

428 

441 

580 

•600 

770 

795 

850 

890 

935 

947 

949 

959 

'964 

967 

975 

1,020 

1,035 

1,055 

1,058 

1,098 

1,100 

1,125 

1,146 

1,245 

1,260 

1,320 

1,347 

1,370 

1,390 

1,400 

1,415 

1,435 

1,445 


,465 

473 

,478 

,495 

,505 

,522 

,535 

,540 

1,575 

1,595 

1,605 

1,630 

1,673 

1,675 

1,679 

1,700 

1,710 

1,715 

1,727 

1,733 

1,733 


Bport.  sec.  36,  SE.,  No.  2. 

Operators — Snowden  Bros. 
Farm  and  well— E.  Fyffe,  No.  9. 
Elevation — 506  feet. 


12 


Sh 
Lii 

Sh 

Lii 
Sa 
Sh 
Sa 
Sa 
Sh 
Co 
Li: 
Bi 

R€ 

SI; 
Li 
SI; 
Li 


Ss 
Si 

si 
C( 
SI 
Li 
SI 
Si 
SI 
S; 
SI 
L 
SI 
L 
SI 
L 
S; 
SI 
S. 
S 
L 
S 
S; 
S 
L 
S 

s 
s 

L 
S 
L 
S 
P 

s 
I 

c 


BLATCHLEY] 


LAWRENCE    COUNTY    CROSS-SECTIONS. 


m 


Logs — Continued. 


Soil   

Slate    

Limestone    shell 

Slate    

Sand  (water,  240  to  300  feet) 

Slate     

Sand    

Slate     

Limestone,    hard 

Red    slate 

Sand,  white,   hard 

Limestone,   white,   hard 

Slate,    dark,    soft 

Sand,   white,   hard 

Slate    

Limestone,    white,    hard 

Slate     

Limestone     

Slate    

Sand   (water,   905  feet) 

Slate    

Sand    (water,    1,160   feet)  .... 

Slate    

Sand    (water,    1,325   feet)  .... 

Slate    

Sand    (water,    1,435   feet)  .... 

Limestone     

Slate,    dark 

Red  rock,  cave 

Slate,    dark,    soft 

Slate,    dark,    hard 

Sand,    white,    hard 

Slate,    white*    soft 

Shale    

Sand    (water,    1,589 V2    feet).. 

Limestone    

Slate,    black 

Slate,    white 

Red    slate 

Shell,   hard 

Sand,  white    (oil,   1,651  feet). 
Slate,    dark 

Total    depth 

Initial  production,  150  bbls. 


Thickness 

Depth 

Feet 

Feet 

14 

14 

90 

104 

10 

114 

111 

225 

85 

310 

55 

365 

40 

405 

10 

415 

12 

427 

10 

437 

15 

452 

7 

459 

192 

651 

11 

662 

838 

2 

840 

858 

7 

865 

25 

890 

50 

940 

1,125 

135 

1,260 

25 

1,285 

40 

1,325 

1,390 

60 

1,450 

1,460 

43 

1,503 

1,510 

5 

1,515 

17 

1,532 

7 

1,539 

1,554 

19 

1,573 

1,589 

20 

1,609 

1,629 

9 

1,638 

2 

1,640 

2 

1,642 

57 

1,699 

18% 

1,717% 

1,717% 


Bport.  sec.  31,  NW.,  No.  14. 


Operators — Central  Refining  Company. 
Farm  and  well — Perry  King,  No.  5. 
Elevation— 487  feet. 


Thickness  Depth 

Feet  Feet 

Clay     70  70 

Limestone     6  76 

Slate     20  96 

Limestone     14  110 

Slate    35  145 

Limestone     5  150 

Sand    80  230 

Limestone     : 30  260 

Sand    45  305 

Slate    10  315 

Sand    10  325 

Red    rock 6  331 

Limestone     20  351 

Slate    174  525 

Sand    12  537 

Slate 158  695 

Sand    30  725 

Slate     55  780 

Limestone     5  785 

Sand    80  865 

Slate  and  shells 115  980 

Sand   (show  of  oil,  995  feet) 60  1,040 


128 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


Logs — Continued. 


Thickness  Depth 

Feet  Feet 

Slate     12  1,052 

Sand    83  1,135 

Slate 10  1,145 

Sand    145  1,290 

Slate    15  1,305 

Sand    35  1,340 

Slate    10  1,350 

Red    rock 12  1,362 

Limestone     53  1,415 

Red   rock 6  1,421 

Sand    15  1,436 

Limestone     29  1,465 

Slate    14  1,479 

Red   rock 15  1,494 

Sand    (oil) 30  1,524 

Total    depth 1,524 


Pet.  sec.  80,  SE.,  No.  26. 

Operators — Bridgeport  Oil  Company. 

Farm  and  well— Willey,  No.  11. 

Elevation — 507  feet. 

Thickness 
Feet 

Soil     6 

Quicksand    .           .  .  9 

Slate 85 

Sand    25 

Limestone,  hard \  , 7 

Sand    18 

Slate   and   limestone 85 

Sand    5 

Coal     3 

Slate  and   limestone 12 

Red    rock 20 

Limestone  and  slate 85 

Sand    .  .  . 30 

Slate   and'  limestone 84 

Coal    2 

Slate  and   limestone 134 

Sand    28 

Slate   and   limestone 67 

Salt  sand 45 

Slate   and   limestone 45 

Sand   (oil,  820  feet) 35 

Limestone    10 

Slate    15 

Limestone    103 

Slate    5 

Sand,   broken 26 

Sand   (show  of  oil,   1,000  feet) 16 

Slate    10 

Sand    25 

Slate    10 

Limestone     15 

Sand    40 

Limestone     10 

Salt    sand 57 

Limestone    6 

Slate    21 

Sand    9 

Slate    7 

Red   rock 10 

Limestone    5 

Slate     20 

Limestone    15 

Slate    2 

Limestone    8 

Slate    15 

Sand    (gas) 10 

Limestone     18 

Slate 36 

Sand    (oil,   1,358   feet) 8 

Slate     

Total    depth 


Depth 

Feet 

6 

15 

100 

125 

132 

150 

235 

240 

243 

255 

275 

360 

390 

474 

476 

610 

638 

705 

750 

795 

830 

840 

855 

958 

963 

989 

1,005 

1,015 

1,040 

1,050 

1,065 

1,105 

1,115 

1,172 

1,178 

1,199 

1,208 

1,215 

1,225 

1,230 

1,250 

1,265 

1,267 

1,275 

1,290 

1,300 

1,318 

1,354 

1,362 

1,362 

1,362 


blatchley]                   LAWEENCE   COUNTY   CEOSS-SECTIONS.  129 

Logs — Continued. 

Pet.  sec.  29,  NW.,  No.  39. 

Operators — Silurian  Oil  Company. 
Farm  and  well — J.  D.  Bowers,  No.  7. 
Elevation— 443  feet. 

Thickness        Depth 

Feet  Feet 

Sand   (oil,   920  feet) 75  910   to      985 

Sand    (salt   water) 40  1,060  to  1,100 

Slate 38  1,138 

Red    rock 4  1,142 

Slate    32  1,174 

Limestone    12  1,186 

Slate    39  1,225 

Limestone    15  1,240 

Slate    25  1,265 

Red    rock 5  1,275  to  1,280 

Slate     8  1,288 

Sand    32  1,320 

Slate     35  1,355 

Limestone    15  1,370 

Slate    50  1,420 

Sand    (gas,    1,427    feet) 15  1,425   to  1,440 


Total    depth 1,440 

Gas  well,   520  pounds  rock  pressure. 

Pet.  sec.  29,  NW.,  No.  8. 

Operators — Bridgeport  Oil  Company. 
Farm  and  well — Eshelman,  No.  16. 
Elevation — 438  feet. 

Thickness  Depth 

Feet  Feet 

Soil     25  25 

Sand 47  72 

Slate    53  125 

Sand    20  145 

Slate    10  155 

Sand    10  165 

Slate     5  170 

Limestone    5  175 

Slate 60  235 

Limestone    10  245 

Slate     15  260 

Sand    40  300 

Limestone     5  305 

Slate    45  350 

Sand 15  365 

Slate    42  407 

Coal     3  410 

Slate    , 90  500 

Sand    20  520 

Slate    55  575 

Limestone,     hard 5  580 

Slate    5  585 

Sand,    broken 81  666 

Slate,    soft 24  690 

Limestone    10  700 

Slate    60  760 

Limestone    15  775 

Sandy    limestone 27  802 

Slate,  black 58  860 

Sand    (oil) 10  870 

Broken   sand 52  922 

Sand  (some  oil,  925  feet),  white 58  980 

Slate    7  987 

Limestone    11  998 

Slate     7  1,005 

Limestone,    hard 10  1,015 

Slate    10  1,025 

Limestone    10  1,035 

—9  G 


130  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

Logs — Concluded. 


Slate    

Sand    (salt  water) 

Limestone    

Slate    

Sandy    limestone 

Limestone   

Red    rock 

Slate    

Limestone     

Slate    

Red   rock 

Slate    

Sand    (gas) 

Limestone,    hard 

Slate    

Red   rock 

Sand   (oil  pay,   1,298  to  1,330  feet) 

Slate    

Limestone     

Slate    

Limestone    

Total    depth 


Thickness 

Depth 

Feet 

Feet 

15 

1,050 

55 

1,105 

5 

1,110 

6 

1,116 

13 

1,129 

15 

1,144 
1,146 

2 

34 

1,180 

18 

1,198 

12 

1,210 

13 

1,223 

4 

1,227 

13 

1,240 

10 

1,250 

1,273 

12 

1,285 

1,348 

25 

1,373 

1,387 

33 

1,420 

1,426 

1,426 

Pet.  sec.  20,  SE.,  No.  7. 


Operators — E.  N.  Gillespie. 
Farm  and  well — Smith,  No.  24. 
Elevation — 435  feet. 


Sand    (salt   water) 
Slate    and    shells.  . 

Sand    

Sand    (water) 

Slate    

Sand,    salt 

Slate  and  shells. . . 

Red   rock 

Slate    

Limestone    

Slate    

Shells    and    slate.  . 

Sand,    broken 

Sand     (oil) 

Slate     

Sand    

Limestone    

Slate    


Thickness 

Depth 

Feet 

Feet 

25 

725 

251 

976 

5 

981 

94 

1,075 

95 

1,170 

86 

1,256 

41 

1,297 

13 

1,310 

10 

1,320 

30 

1,350 

35 

1,385 

52 

1,437 

27 

1,465 

10 

1,475 

8 

1,483 

56 

1,539 

5 

1,544 

17 

1,561 

Total    depth 1,561 

Initial  production,   80  bbls. 

Cross-section  D-D. 

The  D-D  cross-section,  PL  XV,  is  drawn  across  the  southern  end  of  the 
field.  It  shows  the  flattened  nature  of  the  LaSalle  anticline  in  this  re- 
gion and  the  small  terrace  on  the  western  limb  of  the  fold.  The  "Gas" 
sand  is  not  noted  in  this  portion  of  the  field.  The  remaining  producing 
sands  are  essentially  flat  but  locally  irregular.  The  section  is  made  up 
of  the  following  records: 

LOGS. 

The  records  of  the  following  wells  are  in  the  tables  of  well  data: 


blatchley]  LAWRENCE    COUNTY    CROSS-SECTIONS. 

Logs — Continued. 
List  of  Wells  Affording  Data  for  Cross-Section  D-D. 


131 


Township. 

Section. 

Quarter- 
section. 

Well 
number. 

29 

NE. 
SW. 

sw. 

NW. 

NE. 

NE. 

NW. 

SW. 

SE. 

SE. 

SE. 

NW. 

NW. 

NE. 

NE. 

SW. 

2 

21...                                         

2 

21..                                   

3 

21 

6 

21..                                                               

9 

21 

10 

22 

12,   13 

Lawrence 

15 

17 

15 

1 

15 

9 

15 

12 

14 

7 

14 

3 

14 

17 

14 

1 

12 

8 

The  remaining  detailed  logs  of  the  section  are  presented  below  and 
elsewhere  in  this  report: 


Bport.  sec.  80,  NE.,  No.  2. 

Operators — Snowden  Bros. 
Farm  and  well — McOrr,  No.  1. 
Elevation— 503  feet. 

Thickness  Depth 

Feet  Feet 

Soil  and  slate 80  80 

Sand,  white    (water,   80   feet) 35  125 

Slate,    white,    soft 105  230 

Sand    30  260 

Slate    10  270 

Limestone    4  274 

Slate    156  430 

Limestone    8  438 

Slate,  red,  soft 7  445 

Slate,  white,  soft 15  460 

Sand    15  475 

Slate    125  600 

Coal 4  604 

Slate    71  675 

Sand,  white,   hard 5  680 

Slate    90  770 

Limestone    15  785 

Slate,    white,    soft 83  868 

Sand,  white,  soft   (hole  full  of  water,  916  feet) 48  916 

Slate,    dark,    soft 25  941 

Limestone,   white,   hard 9  950 

Slate    20  970 

Limestone    , 8  978 

Slate     19  997 

Sand    3  1,000 

Slate    40  1,040 

Sand,  white,  soft   (water,   1,045  feet) 15  1  055 

Slate     20  1,075 

Limestone,   white,  very  hard 3  1,078 

Slate,    dark,    soft 42  1120 

Sand,  white,  soft   (hole  full  of  water,   1,170  feet) ....'.'.  210  L330 

Slate,    dark 53  1,383 

Sand,  light,  hard 9  1  392 

Slate,    dark,    soft 23  l'415 

Sand,  white    (water,   1.420   feet) 35  i',450 

Slate,    dark,    soft 70  1  520 

Sand   (hole  full  of  water,   1,522  feet) 25  l'545 

Slate    49  i'594 

?and     .  .  . 59  1,653 

Limestone,   white,   hard 15  1668 


132  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 

Logs — Continued. 


Slate,    dark,    loose 

Sand,  dark,  soft  (8  bailers  of  water,  1,708  feet) , 

Slate    

Limestone,   white,   hard 

Red    rock ; 

Slate,    light 

Limestone    

Slate,   dark,   very  soft , 

Limestone    

Slate,   dark,   very  soft 

Sand,  light,  hard 

Slate    

Limestone    , 

Slate    

Sand  (4  bailers  of  water,  1,880  feet) , 

Slate    

Sand  (pay,  1,962  to  1,972  feet) 

Total    depth 1,972 


Thickness 

Depth 

Feet 

Feet 

19 

1,687 

21 

1,708 

5 

1,713 

2 

1,715 

10 

1,725 

13 

1,738 

2 

1,740 

14 

1.754 

10 

1,764 

26 

1,790 

10 

1,800 

8 

1,808 

20 

1,828 

37 

1,865 

1,936 

22 

1,958 

14 

1,972 

Bport.  sec.  29,  NW.,  No. 


Operators — Snowden  Bros. 

Farm  and  well— H.  K.  Seed,  No.  2. 

Elevation — 490  feet. 


Soil    

Sand,  slate  and  shells 

Sand,  white,  soft 

Slate  and  shells 

Slate,   white 

Slate,    dark 

Sand,  white   (salt  water,  851  feet) 

Slate,  sand,  and  shells   (salt  water,  1,165  feet) 

Sand,    white 

Slate,    dark 

Sand    

Limestone,   white 

Slate,    dark 

Sand,   white 

Slate    

Sand,  white  (salt  water,  1,650  feet) 

Red    slate 

Limestone    shells 

Sand    

Slate    and    shells 

Red   rock 

Slate    

Sand,    white 

Slate    

Sand,  white   (salt  water,  1,860  feet) 

Slate     

Shells,    hard 

Sand,    brown _ 

Total    depth 1,900 

Initial  production,  125  bbls. 

Bport.  sec.  29,  NW.,  No.  1. 

Operators — Snowden  Bros. 

Farm  and  well — H.  K.  Seed,  No.  1. 

Elevation — 476  feet. 

Thickness  Depth 

Feet  Feet 

Red   rock 5  415 

Sand,    dry 14  610 

Slate     150  760 

Sand    15  775 


Thickness 

Depth 

Feet 

Feet 

18 

18 

332 

350 

50 

400 

300 

700 

50 

750 

81 

831 

129 

960 

205 

1,165 

105 

1,270 

25 

1,295 

25 

1,320 

25 

1,345 

80 

1,425 

187 

1,612 

8 

1,620 

30 

1,650 

25 

1,675 

55 

1,730 

20 

1,750 

35 

1,785 

6 

1,791 

11 

1,802 

26 

1,828 

17 

1,845 

20 

1,865 

14 

1,879 

2 

1.881 

17 

1,898 

L33 


830 
870 
880 
920 
930 
950 
045 
275 
300 
450 
490 
510 
530 
537 
700 
705 
800 
815 
830 
858 
860 
862 
874 
885 

885 


:et 
90 
.07 
.45 
.55 
.65 
!65 
178 
;50 
20 
10 
00 
05 
20 
80 
65 
80 
90 
00 
16 
22 
30 
85 
29 
59 
90 
00 
05 
21 
44 


132 


Slate,  dai 
Sand,  dar 
Slate  .... 
Limestone 
Red  rock 
Slate,  lig] 
Limestone 
Slate,  dar 
Limestone 
Slate,  dar 
Sand,  ligh 

Slate    

Limestone 

Slate    

Sand   (4  b 

Slate    

Sand  (pay 

Total 


Operato 
Farm  a 
Elevatn 


Soil    

Sand,  slate 
Sand,  whit 
Slate  and  i 
Slate,  whit 
Slate,  darl 
Sand,  whit 
Slate,  sand 
Sand,  whit 
Slate,    dart 

Sand    

Limestone, 
Slate,    dart 
Sand,   whit 

Slate    

Sand,  whit< 
Red  slate . 
Limestone 

Sand    

Slate    and 
Red    rock. . 

Slate    

Sand,    whit< 

Slate    

Sand,  white 

Slate     

Shells,  har 
Sand,    brew 

Total    ( 
Initial  pr< 


Operator 
Farm  an 
Elevatioi 


Red   rock . . 
Sand,    dry. 

Slate     

Sand    


BLATCHLEY] 


LAWKENCE    COUNTY    CROSS-SECTIONS. 


133 


Logs — Continued. 


Thickness        Depth 


Slate    

Sand    (salt  water,  840  and  880  feet) 

Slate    

Sand    (water) 

Slate    

Sand    (water) 

Slate    

Sand    (water) 

Limestone 

Slate    

Sand    (water,   1,460   feet) 

Slate    

Limestone    

Sand    

Slate    

Red   rock 

Slate    

Red    rock 

Sand    (water,    1,830   feet) 

Slate    

Limestone    

Slate    

Oil    sand 

Slate    

Total    depth 

Initial  production,  40  bbls. 


Feet 

Feet 

55 

830 

40 

870 

5 

875  to   880 

40 

920 

10 

930 

20 

950 

95 

1,045 

230 

1,275 

25 

1,300 

150 

1,450 

40 

1,490 

20 

1,510 

20 

1,530 

5 

1,532  to  1,537 

163 

1,700 

5 

1,705 

95 

1,800 

15 

1,815 

15 

1,830 

28 

1,858 

2 

1,860 

2 

1,862 

12 

1,874 

11 

1,885 

1,885 

Law  sec.  11,  SE.,  No.  6. 
Presented  in  the  stratigraphic  discussion,  page  67. 

Law.  sec.  12,  SW.,  No.  7. 
Presented  in  the  stratigraphic  discussion,  page  68. 

Law.  sec.  12,  SW.,  No.  4. 

Operators — Bridgeport  Oil  Company. 
Farm  and  well — Henry,  No.  1. 
Elevation— 440  feet. 


Soil,   etc 

Sand    (fresh  water) 

Slate    

Limestone    

Slate    

Limestone    shells 

Red   rock 

Limestone,  slate,  and  shells 

Slate,  pencil  cave 

Limestone  and  slate 

Sand  (hole  full  of  salt  water,  700  feet) . 

Slate   and    shells 

Sand  (salt  water,  910  feet) 

Slate    

Sand   (salt  water,   1,000  and  1.030  feet) 

Slate,    black 

Slate    and   shells 

Limestone    

Sand   (water,   1,300   feet) 

Slate    

Sand    

Limestone 

Slate  and  shells 

Limestone     

Slate    

Red  rock,  cave 

Slate    

Lime    

Slate    


Thickness 

Depth 

Feet 

Feet 

90 

17 

107 

38 

145 

10 

155 

10 

165 

100 

265 

13 

278 

72 

350 

70 

420 

190 

610 

90 

700 

205 

905 

15 

920 

60 

980 

85 

1,065 

115 

1,180 

110 

1,290 

10 

1,300 

16 

1,316 

6 

1,322 

8 

1,330 

55 

1,385 

44 

1,429 

30 

1,459 

31 

1,490 

10 

1,500 

5 

1,505 

16 

1,521 

23 

1,544 

134  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 

Logs — Concluded. 

Thickness  Depth 

Feet  Feet 

Red    rock 5  1,549 

Sand   (oil,  1,556  and  1,568  feet) 31  1,580 

Slate    10  1,590 

Sand  (show  of  oil) 5  1,595 

Slate    5  1,600 

Sand    (oil   pay) 10  1,610 

Limestone    shell 90  1,700 

Red    rock,    cave 10  1,710 

Limestone 77  1,787 

Sand 4  1,791 

Limestone    91  1,882 

McClosky    sand 6  1,888 

Total    depth 1,889 

Law.  sec.  12,  SE.,  No.  2. 

Operators — Bridgeport  Oil  Company. 
Farm  and  well — Tracey  Heirs,  No.  1. 
Elevation — 455  feet. 

Sand  (water  at  12  feet.) 

Sand  and  gravel , 

Slate    

Sand     , 

Limestone    

Sand    

Limestone    , 

Slate    

Limestone    

Slate    

Limestone     

Slate    

Sand    

Limestone    

Slate    

Limestone    

Slate    

Limestone    

Slate 

Limestone    

Slate    

Sand    (water ) 

Slate    

Limestone    

Slate    

Sand    

Slate 

Limestone    

Slate    

Sand    

Slate    

Sand    (water) 

Slate    

Sand     

Slate    

Limestone     

Slate    

Sand  (show  of  oil,  1,285  feet) 

Slate 

Sand     

Slate    

Limestone    

Slate    

Red    rock 

Limestone    

Sand    

Slate    

Sand    (water,    1,570   feet) 

Slate    

Sand  (show  of  oil,  1,595  feet.     Water,  1,600  feet) 

Slate 

Limestone    

Sand    

Limestone    

Well  plugged  and  abandoned. 


Thickness 

Depth 

Feet 

Feet 

85 

85 

15 

100 

10 

110 

10 

120 

30 

150 

5 

155 

85 

230 

12 

242 

48 

290 

10 

300 

15 

315 

25 

340 

12 

352 

48 

400 

10 

410 

50 

460 

15 

475 

103 

578 

5 

583 

17 

600 

30 

630 

50 

680 

30 

710 

13 

723 

12 

735 

80 

915 

5 

920 

27 

947 

63 

1,010 

31 

1,041 

29 

1,070 

15 

1,085 

40 

1,125 

68 

1,193 

15 

1,208 

57 

1,265 

47 

1,312 

48 

1,360 
1,405 

45 

1,425 
1,450 

25 

1,480 

10 

1,490 

1,500 

10 

1,510 

1,565 

20 

1,585 

1,590 
1,615 

25 

1,727 

45 

1,772 

1,786 

297 

2,083 

BLATCHLET] 


RELATIONS  OF  STRUCTURE  TO  OIL  AND  GAS. 


135 


RELATIONS  OF  STRUCTURE  TO  OIL  AND  GAS. 


Oil. 

The  oil  sands  of  Lawrence  county  have  proven  the  richest  in  Illinois. 
They  show  remarkable  stability  in  their  yield  and  have  promise  of  long 
life.  The  shallower  sands  have  declined  rapidly,  but  the  Kirkwood, 
Tracey  and  McClosky  sands  are  still  prolific.  Of  the  2,810  wells  mapped 
in  this  county,  but  156,  or  5%  per  cent  were  dry.  There  are  890  wells 
mapped  in  Petty  township,  860  in  Bridgeport,  349  in  Lawrence,  and 
711  in  Dennison.  The  range  of  initial  production  is  between  one  and 
2,400  barrels  per  day.  The  Kirkwood  sand  has  shown  the  best  general 
production  while  the  McClosky  sand  yielded  the  greatest  number  of 
gushers.  The  Bridgeport  sand  is  the  second  best  general  producing 
sand.  It  has  declined  rapidly,  however,  and  is  giving  way  to  the 
development  of  steadier  sands  beneath.  There  are  1,835  of  the  2,654 
producing  wells,  or  about  70  per  cent,  that  furnish  information  of  the 
initial  yield.  This  is  sufficient  to  indicate  the  nature  of  distribution  of 
oil  in  this  field  with  respect  to  structural  conditions.  The  following 
table  shows  the  number  of  wells  that  furnished  data  of  initial  produc- 
tions for  each  sand.  They  are  listed  by  townships,  sands,  and  extent  of 
yield.     The  gas  and  dry  wells  are  also  given: 


Table  Showing  Initial  . 

Productions 
County 

of  Various  Sands  in  the 
Field. 

Lawrence 

Lawrence  county. 

Number  of  wells  classified  according  to  their  initial  production. 

Township. 

Producing  sand. 

0-10 
bbls. 

10-50 
bbls. 

50-100 
bbls. 

100-200 
bbls. 

200-500 
bbls. 

Over 

500 

bbls. 

Gas. 

Dry. 

Petty 

Bridgeport 

4 

27 

19 

21 

15 

1 

"Gas" 

13 
71 
20 
52 

48 
4 
7 

60 
1 
5 

1 

7 

6 
87 
15 
35 

100 

8 
2 

74 
1 

13 

1 
11 

3 
63 

7 
23 

47 

30 

3 

47 

1 

3 

4 
51 

3 
8 

22 
5 

...... 

"  Y 

8 

Kirkwood 

4 
2 

8 

6 

10 
1 

4 

3 
38 

1 
19 

4 
6" 

3 

8 

4 

Tracey 

McClosky 

44 

Bridgeport. . . 

Bridgeport 

Kirkwood 

4 

Tracey 

McClosky 

6 

4 

22 

Lawrence 

Bridgeport 

Buchanan 

22 

1 

"Gas" 

Kirkwood 

3 

44 
8 
2 

4 

50 

1 

27 
1 
4 

21 

6 

Tracey 

McClosky . .     . 

1 

4 

5 

4 

25 

Shallow 

Bridgeport 

5 
1 

51 
3 

54 
22 

9 
10 

9 

Buchanan 

"Gas" 

\ 

Kirkwood 

12 
3 

65 
5 
4 

4 
126 
12 
20 
240 
34 
63 

76 
4 
5 

38 
2 

7 

11 
1 
6 



16 

1 
1 

Tracey 

McCloskv 

65 

Total  for  field. 

Shallow 

Bridgeport 

15 

1 

171 

22 

8 

264 
21 
57 

126 

103 

6 

169 

10 
37 

27 
70 

1 
46 

2 
21 

3 
9 

8* 

30" 

10 

6" 

9 
24 
13 

"Gas" 

Kirkwood 

3 
5 
9 

Tracer 

McCloskv 

156 

136 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


PETTY    TOWNSHIP. 

The  oil  in  sections  25,  26,  35  and  36,  at  the  extreme  northern  end  of 
the  county,  comes  from  the  McClosky  and  Tracey  sands.  The  initial 
yield  per  well  does  not  exceed  200  barrels.  The  oil  in  both  sands  is 
found  under  a  small  dome  on  the  top  of  the  fold,  which  is  separated 
from  the  elongated  dome  farther  south  by  a  narrow  barren  depression 
across  the  field.  The  McClosky  sand  is  highly  productive  along  a  nar- 
row strip  north  and  south  through  the  center  of  the  field,  especially  in 
sections  18  and  30.  The  largest  initial  productions  of  Lawrence  county 
were  found  in  this  sand  in  section  18.  The  oil  is  crowded  into  a  small 
dome,  similar  in  height,  extent,  and  altitude  to  the  arch  in  the  extreme 
northern  end  of  the  field.  The  same  sand  is  productive  at  a  like  alti- 
tude on  the  western  flank  of  the  dome-like  structure  in  section  30.  The 
productive  strip  is  very  narrow  through  this  section  but  becomes  broader 
in  sections  31  and  6,  Bridgeport  township. 

The  Kirkwood  sand  shows  the  greatest  number  of  producing  wells  in 
the  remaining  sections  of  the  field,  especially  along  the  eastern  dip  of  the 
anticline  in  sections  20  and  29.  The  wells  in  this  region  reported  ex- 
cellent initial  productions.  The  Kirkwood  sand  is  also  highly  produc- 
tive in  section  30,  between  30  and  80  feet  lower  than  the  crest  on  the 
west  side  of  the  dome. 

The  "Gas"  sand  primarily  produces  gas  but  is  productive  of  oil  in 
the  following  wells : 

List  of  Wells  Producing  Oil  From  the  'Gas'  Sand;  Lawrence  County. 


Township. 

Section. 

Quarter- 
section. 

Number 
of  well. 

Initial 
production 
in  bbls. 

Petty 

1 

NE. 
NW. 

sw. 
sw. 
sw. 

NE. 

sw. 

3E. 
SE. 

SE. 
SW. 
SW. 

NW. 

NE. 

SE. 

NW. 

NE. 

NE. 

NE. 

NE. 

NW. 

NW. 

NE. 

NE. 

NE. 

SE. 

NE. 

NE. 

SW. 

9 
9 
1 
4 

17 

2 

9 

6 

7 

•      2 

5 

6 

1 

2 

7 

9 

19 

22 

23 

9 

26 

27 

55 

56 

59 

4 

5 

18 

6 

20 

7        

40 

7     .                                

45 

7                                        

35 

7 

15 

12...           . 

65 

12  ..               

75 

12                           

135 

12                       

110 

13                         

75 

17     

35 

17     

25 

20                  

25 

24                    

40 

24                        

20 

5                    

170 

6                      

70 

6                       

30 

6                       

45 

8                        

60 

8                          

50 

8                   

30 

- 

31                        

100 

31                        

100 

31                   

250 

31                   

50 

32                    

105 

32                    

20 

32                           

25 



The  Buchanan  sand  appears  unproductive  in  Petty  township.  It  is 
not  correlated  in  this  region  because  of  possible  confusion  with  the 
Bridgeport  lenses.     In  fact,  it  may  be  possible  that  some  of  the  lower 


blatchlet]  RELATIONS  OF  STRUCTURE  AND  OIL.  137 

productive  lenses  of  the  Bridgeport  sand  are  mistaken  for  the  Buchanan. 
The  Bridgeport  sand  is  especially  productive  in  sections  18,  19,  20,  29 
and  30.     The  initial  yields  are  between  30  and  300  barrels. 

BRIDGEPORT   TOWNSHIP. 

The  Bridgeport,  Buchanan,  and  Kirkwood  sands  are  the  most  pro- 
ductive in  Bridgeport  township.  The  Bridgeport  and  Kirkwood  sands 
have  the  largest  number  of  average  size  wells,  while  the  Buchanan  sand 
has  the  larger  number  of  gushers. 

The  Bridgeport  sand  is  especially  productive  in  sections  32,  5  and  8, 
which  lie  structurally  along  the  southern  slope  of  the  double  plunging 
anticline.  The  average  yield  in  these  sections  is  between  50  and  150 
barrels. 

The  Buchanan  sand  has  its  type  area  in  section  17.  The  wells  are 
very  rich  in  their  initial  yield,  varying  between  100  and  over  500 
barrels.  There  are  a  number  of  gushers  recorded  from  this  locality. 
The  oil  is  crowded  into  a  small  dome  on  the  crest  of  the  anticline; 
the  structure  is  discussed  on  page  107. 

The  Kirkwood  sand  yields  the  best  wells  in  sections  6,  31  and  32, 
which  lie  along  the  western  flank  of  the  arch  and  the  south-western 
slope  of  the  largest  dome. 

The  McClosky  sand  is  productive  in  sections  6  and  31.  This  is  an 
extension  of  the  narrow  productive  area  through  Petty  township.  Sev- 
eral gushers  are  reported  from  section  31. 

LAWRENCE    TOWNSHIP. 

The  Kirkwood  and  Buchanan  sands  are  the  most  productive  in 
Lawrence  township.  This  locality  is  the  type  area  for  the  Kirkwood 
and  a  portion  of  the  Buchanan  sands. 

The  Buchanan  sand  is  especially  productive  in  sections  15  and  16. 
The  average  yield  is  100  to  200  barrels.  Several  large  wells  are  reported 
from  this  area.  The  oil  is  crowded  into  a  dome  similar  in  height  and 
altitude  to  the  one  in  section  17,  Bridgeport  township. 

The  type  locality  for  the  Kirkwood  sand  lies  in  sections  13  and  14 
and  extends  southward  into  Dennison  township.  The  wells  are  not 
highly  productive.  The  oil  lies  in  an  extensive  flat  in  the  sand  which 
spreads  southward  through  the  remainder  of  the  field.  The  McClosky 
sand  shows  a  number  of  excellent  wells  in  section  14. 

DENNISON   TOWNSHIP. 

The  Bridgeport,  Kirkwood  and  McClosky  are  the  prominent  pro- 
ducing sands  of  Dennison  township.  The  Kirkwood  sand,  as  in 
Bridgeport  and  Petty  townships,  is  the  most  widely  productive.  The 
Bridgeport  sand  closely  follows  the  Kirkwood  sand  in  yield  but  is 
spotted  in  its  distribution.  The  McClosky  formation  has  furnished 
the  best  producing  wells. 

The  Bridgeport  sand  is  especially  productive  in  sections  2,  26,  34 
and  35.  This  area  lies  along  the  southwestern  edge  of  the  field.  The 
wells  average  50  to  150  barrels  initial  yield. 


138 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


The  Buchanan  sand  is  notably  productive  only  in  section  21,  which 
is  an  extension  of  the  small  dome  lying  in  sections  15  and  16,  Lawrence 
township.     The  wells  "are  exceptionally  large  in  their  initial  yield. 

The  Kirkwood  sand  shows  many  wells  in  sections  22,  23,  25,  26,  35 
and  36.  The  initial  yield  averages  100  barrels.  The  oil  lies  over  a 
broad  flat  in  the  sand  that  covers  most  of  Dennison  township. 

The  Tracey  sand  shows  a  light  production  in  sections  25  and  26. 

The  McClosky  sand  has  its  type  area  and  best  production  in  section 
25.  There  are  many  gushers  from  the  McClosky  sand  in  this  section, 
the  highest  reporting  1,860  barrels  for  the  first  day.  The  productive 
areas  of  this  sand  lie  at  an  altitude  of  about  160  feet  above  the  datum 
plane. 

Gas. 

There  are  about  70  gas  wells  in  Lawrence  county.  Gas  is  reported 
incidentally  in  over  half  of  the  records  and  is  widely  distributed  in  all 
the  sands.  The  Kirkwood,  Tracey  and  McClosky  sands  have  yielded 
the  most  gas,  particularly  in  Petty  township  where  the  field  is  governed 
by  an  elongated  dome.  The  following  table  shows  the  locations  and  all 
available  production  data  of  the  gas  wells  in  Lawrence  county: 


Locations  of  Gas  Wells  in  Lawrence  County,  and  Sources  of  Gas. 


Township. 

Section. 

Quarter- 
section. 

Well 
number. 

Name  of  sand. 

Yield  in 

cu.  ft. 
per  day. 

Remarks. 

1 

NW. 

sw. 

NE. 

NE. 

NE. 

NE. 

NW. 

SE. 

SE. 

NW. 

SW. 

NE. 

NE. 

NW. 

NW. 

NW. 

SE. 

SE. 

NE. 

NW. 

NW. 

SE. 

SE. 

SW. 

NW. 

NE. 

SW. 

SW. 

NW. 

SE. 

NE. 

SW. 

SW. 

SW. 

SE. 

SE. 

SE. 

NW. 

NW. 

6 
3 
2 
4 
6 
7 
1 
2 
5 
10 
9 
4 
5 
1 
2 
7 
1 
9 
4 
2 
6 
6 

29 

29 

3 

7 

4 

5 

39 

1 

24 

6 

9 

13 

31 

59 

69 

9 

12 

Tracey 

1 

2 

2 

' 

Kirkwood 

4,000,000 

Second  lens 

2 

McClosky 

2,500,000 

2 

2 

do 

2 

..do 

7,000,000 

600  pounds  pressure 

2 

..do 

Tracey 

Second  lens 

7 

7 

..do 

12... 

12 

Tracey 

12 

do 

12 

do 

12.... 

do 

12  . 

..do 

12     . 

do 

13  . 

19  . 

3,000,000 
7, 500, 000 

19  . 

do 

650  pounds  pressure 
400  pounds  pressure 

19 

do 

19.... 

"Gas" 

20..     . 

Bridgeport. . . 

24..   . 

Second  lens 

25..    . 

T.  5N.,  R.  13  W... 

2>..  . 

do 

do 

25 

..do 

..do 

29..    . 

..do 

520  pounds  pressure 

29 

"Gas".... 

30 

30 

30 

30 

30 

do 

30 

McClosky 

do 

6, 000, 000 
2,000,000 

30 

36 

..do 

Kirkwood 

T.  5N.,  R.  13  W... 

36 

..do 

BLATCHLET]  .RELATIONS  OF  STRUCTURE  AND  GAS.  139 

Locations  of  Gas  Wells  in  Lawrence  County — Concluded. 


Township. 

Section. 

Quarter- 
section. 

Well 
number. 

Name  of  sand. 

Yield  in 

cu.  ft. 

per  day. 

Remarks. 

Bridgeport 

8        

NW. 

NE. 
NE. 
NE. 
NE. 
SE. 
SE. 
SE. 

sw. 

SW. 

SW. 

SW. 
SW. 

SE. 

SE. 

NE. 

NE. 

NE. 

NE. 

NW. 

NW. 

SE. 

29 

7 

23 

48 

50 

6 

11 

14 

6 

10 

24 

2 

6 

3 

4 

2 

5 

6 

4 

7 

8 

1 

Buchanan 

McClosky 

..do 

1,000,000 
1,000,000 

31 

31 

31 '.. 

..do 

31 

..do 

31 

"Gas" 

31 

McClosky 

31 

"Gas" 

32 

..do 

1,000,000 

32 

McClosky 

32    .           

Kirkwood 

1 

Tracey 

4, 500, 000 
3,000,000 

1 

Kirkwood 

Bridgeport 

Second  lens 

27 

27 

..do 

34 

do 

34 

..do 

34 

..do 

35  .. 

..do 

2,000,000 

35 

.do 

35 

do 

35 

Shallow 

2,500,000 

PETTY    TOWNSHIP. 

The  greatest  number  of  gas  wells  of  the  Lawrence  county  field  lie  in 
Petty  township.  They  are  scattered  along  the  flanks  of  the  anticline. 
The  "Gas"  sand  yields  gas  in  small  quantities  over  Petty  township  and 
abundantly  in  section  30.  The  gas  does  not  occur  at  the  apex  of  the 
large  dome  centering  in  this  section  but  lies  about  60  feet  below  on  its 
western  flank.  The  Kirkwood  sand  is  especially  productive  of  gas  in 
sections  1  and  2  in  the  northern  end  of  the  field.  The  gas  seems  to  be 
arrested  along  the  steep  western  flank  of  the  anticline.  The  Tracey 
sand  shows  the  greatest  productions  of  gas  in  this  township,  and,  in- 
deed, over  the  entire  area.  The  best  yield  is  in  the  northern  portion 
of  the  township  and  through  the  middle  of  the  broad  fold.  Several 
wells  also  yield  gas  about  120  feet  below  the  apex  of  the  dome  in  sec- 
tion 30.  The  McClosky  sand  shows  an  excellent  yield  of  gas  on  the 
crest  of  the  same  dome. 


Bridgeport  Township. 

The  "Gas"  and  McClosky  sands  yield  the  best  pressures  of  gas  in  the 
northern  end  of  the  township.  The  McClosky  sand  shows  several  good 
wells  in  section  31,  about  70  feet  lower  than  the  crest  of  the  dome. 
The  two  smaller  domes  in  sections  31  and  32  contain  gas.  The  "Gas" 
sand  yields  abundant  gas  in  sections  6  and  31,  but  it  lies  between  100 
and  140  feet  below  the  crest  of  the  dome.  The  Buchanan  sand  usually 
possesses  little  or  no  gas,  but  it  reports  it  in  several  wells  in  sections 
7  and  8.  The  type  locality  of  this  sand,  section  17,  does  not  report  any 
gas.  The  Kirkwood  sand  shows  a  scattered  record  of  gas  in  its  many 
wells,  but  particularly  in  section  17. 


140  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

Lawrence  Township. 

The  Kirkwood  sand  shows  gas  in  most  of  the  wells  in  Lawrence 
township.  The  Bridgeport  and  Buchanan  sands  show  no  gas  while  the 
McClosky  gives  data  from  about  six  wells.  There  are  no  commercial 
gas  wells  in  the  township. 

Dennison  Township. 

The  Bridgeport  sand  shows  a  number  of  gas  wells  in  sections  1,  2,  34 
and  35.  Most  all  the  wells  penetrating  the  Bridgeport  lenses  record  gas 
in  them.  The  Kirkwood  sand  gives  numerous  records  of  gas  over  the 
township  but  particularly  in  sections  22,  23  and  36.  The  McClosky 
sand  shows  abundant  gas  in  sections  25  and  36.  The  gas  would  be 
marketable  from  this  sand  but  for  the  enormous  yield  of  oil. 

RELATIONS  OF  STRUCTURE  TO  SALT  WATER. 

The  sands  of  Lawrence  county  show  abundant  water  along  the  flanks 
of  the  anticline  and  but  little  through  the  center  of  the  field  except  in 
the  lower  Bridgeport  and  Buchanan  sands.  The  Pottsville  rocks  appear 
well  saturated  with  water  over  the  entire  field  and  into  the  limbs  of  the 
LaSalle  fold.  The  Chester  sands  are  not  uniformly  saturated  with 
water  but  seem  to  have  limit  lines  of  saturation  along  the  limbs  of  the 
fold,  more  particularly  along  the  western  side.  The  McClosky  sand 
similarly  shows  abundant  water  on  the  western  slope  of  the  fold  and 
in  parts  of  Petty  township. 

Petty  Township. 

There  is  but  little  water  shown  in  the  record  of  wells  in  the  pro- 
ducing sands  of  Petty  township.  The  Bridgeport  and  Buchanan  sands 
are  closely  associated  and  show  abundant  water  in  sections  1,  2,  19,  20, 
29,  30  and  36.  The  Kirkwood  sand  shows  some  saturation  beneath  the 
oil  in  sections  12  and  36.  The  McClosky  sand  shows  some  water  con- 
tent in  sections  12,  13,  15,  24  and  25. 

Bridgeport  Township. 

All  the  sands  in  sections  1,  18  and  36,  Bridgeport  township  dip  low 
on  the  western  limb  of  the  anticline  and  show  much  water.  The  upper 
Bridgeport  lenses,  like  those  of  the  Robinson  sand  of  Crawford  county, 
are  generally  barren  of  water  within  the  oil  pool  in  this  region.  The 
lower  lenses  are  widely  saturated  in  sections  6,  7,  8,  31  and  32.  The 
Buchanan  sand  is  completely  saturated  with  water  in  sections  6  and  31, 
but  water  underlies  the  oil  zone  in  its  type  locality,  section  17.  The 
Kirkwood  and  McClosky  sands  are  usually  free  from  water  in  this 
region,  except  along  their  outer  edges. 

Lawrence  Township. 

The  Bridgeport  sands  contain  abundant  water  in  Lawrence  township. 
The  Buchanan  sand  is  water-bearing  in  sections  2,  11,  12  and  14,  but 


blatchley]  RELATIONS  OF  STRUCTURE  AND  SALT  WATER.  141 

contains  less  water  and  is  oil-bearing  in  section  16.  No  water  is  reported 
for  this  sand  in  section  15.  The  bottom  of  the  Kirkwood  sand  contains 
water  in  sections  1  and  13.  The  Tracey  sand,  in  several  cases,  shows 
abundant  water  in  section  10.  The  McClosky  sand  is  reported  water- 
bearing only  in  section  1. 

Dennison  Township. 

The  lower  Bridgeport  lenses  and  Buchanan  sand  contain  water  over 
most  of  Dennison  township.  The  upper  lenses  are  productive  at  the 
southern  end  of  the  field  and  show  some  water  beneath  the  oil  in  section 
2.  The  Kirkwood  sand  shows  water  beneath  the  oil  in  sections  1,  5,  6, 
7,  24  and  30.  The  McClosky  sand  is  wet  in  sections  19,  24,  and  in  the 
northern  part  of  25. 


142  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


CHAPTER  V. 


General   Summary  of  Geological  Conditions  in  Crawford  and 
Lawrence   Counties. 


GENEEAL  STATEMENT. 

The  features  of  the  structure  maps  of  the  different  sands,  and  their 
individual  oil,  gas,  and  salt  water  relations  just  described,  are  suffi- 
ciently similar  to  permit  general  conclusions  as  to  the  accumulation  of 
oil  and  gas  in  Crawford  and  Lawrence  counties.  These  conclusions  add 
to  the  general  fund  of  evidence  confirming  the  accumulation  of  oil  and 
gas  in  folded  rocks. 

GENEEAL  STEUCTUEE  OF  EEGlON  OF  THE  LA  SALLE 

ANTICLINE. 

The  greater  portion  of  Illinois  lies  within  the  Eastern  Interior  Coal 
Basin,  which  is,  broadly  speaking,  an  extensive  spoon-shaped  basin,  with 
its  long  axis  extending  along  a  line  through  Cerro  Gordo,  Lovington  and 
Olney  and  with  its  deepest  part  in  Wayne,  Hamilton  and  Edwards 
counties.  The  east  side  of  the  basin  rises  into  a  strong  longitudinal 
fold  known  as  the  LaSalle  anticline,  which  extends  from  the  vicinity 
east  of  LaSalle  in  a  southeastern  direction  to  Sadorous  in  Champaign 
county.  From  thence  it  passes  near  Tuscola  and  enters  the  oil  territory 
of  Clark  county  near  Westfield.  It  continues  in  a  direct  line  through 
the  oil  fields  in  Clark,  Crawford  and  Lawrence  counties  until  the  vicinity 
of  St.  Francisville  in  the  latter  county  is  reached.  The  identity  of  the 
fold  is  lost  beyond  Lawrence  county  but  it  is  thought  to  cross  the 
Wabash  into  Indiana,  and  possibly  merges  into  the  eastern  flank  of  the 
Illinois  basin.  The  writer  has  compiled  several  structure  sections1 
which  illustrate  these  facts. 

The  formations  ascend  from  the  axis  of  the  basin  into  the  Crawford 
and  Lawrence  county  oil  fields  at  the  rate  of  about  50  feet  per  mile. 
The  ascent  becomes  more  rapid  in  Lawrence  county  because  of  the 
presence  here  of  the  very  sharp  apex  of  the  anticlinal  dome. 

The  sands  of  the  Illinois  basin  have  been  thoroughly  tested  im- 
mediately west  of  the  oil  fields  and  found  full  of  salt  water.    The  lower 

i  111.  State  Geol.  Sur  vey,  Bull.  No.  16, 1910,  pis.  7  and  11. 


blatchley]  GEOLOGICAL    SUMMARY.  143 

flanks  of  the  fold  are  known  to  yield  abundant  salt  water  in  all  the 
sands  which  are  productive  in  the  main  fields.  The  conditions  for  the 
accumulation  of  oil  and  gas  in  the  fields  are  ideal  because  of  the  presence 
of  the  following  governing  factors: 

1.  There  is  an  extensive  anticline  with  a  marked  basin  on  at  least 
one  side. 

2.  The  depressions  on  both  sides  of  the  fold,  showing  abundant  water,' 
comprise  extensive  "feeding  areas"  for  the  arch. 

3.  The  sands  are  commonly  porous  and  hence  form  suitable  reser- 
voirs for  the  storage  of  oil. 

4.  There  are  abundant  shales  and  limestones  overlying  the  sand- 
stones which  originally  furnished  the  oil  and  now  probably  serve  as 
impervious  covers  to  the  reservoirs. 

5.  The  sands  in  both  limbs  of  the  anticline  are  abundantly  saturated 
with  salt  water  which  is  probably  instrumental  in  holding  the  oil  and 
gas  captive  in  its  present  position.  This  consideration  is  highly  im- 
portant because  of  the  relations  of  water  and  oil  and  the  resultant  con- 
centration of  oil  in  folded  structure. 

6.  The  portion  of  the  arch  containing  oil  is  six  to  seven  miles  in 
its  extreme  breadth  and  one  or  two  miles  wide  in  the  narrowest  places. 
The  large  amplitude  and  breadth  of  the  arch  offered  an  enormous 
reservoir  capacity. 

DETAILED  FEATURES  OF  THE  FIELDS. 

The  detailed  discussion  of  the  structure  in  the  Crawford  and  Lawrence 
county  field  proves  conclusively  the  presence  of  a  major  fold  governing 
the  accumulation  of  oil  and  gas  in  this  region.  The  crest  of  the  fold, 
however,  is  shown  to  be  very  irregular.  It  is  interrupted  by  numerous 
minor  domes  and  transverse  depressions,  which  perhaps  have  been  in- 
strumental in  segregating  the  pools.  The  succession  of  irregularities 
culminates  in  a  very  extensive  uplift  of  the  axis  of  the  anticline  north 
of  Bridgeport,  Lawrence  county,  which  has  the  appearance  of  an 
elongated  dome.  Other  portions  of  the  anticline  show  a  flattened  crest 
or  minor  domes. 

With  one  exception  the  best  collection  of  oil  was  found  over  the 
extensive  flat  areas  along  the  crest  of  the  parent  fold.  The  large  dome 
in  the  Lawrence  county  field  shows  an  exceptional  accumulation  of  oil 
around  its  flanks  but  not  at  the  crest.  The  domes  over  the  entire  area 
investigated  are  logical  gas  reservoirs.  The  gas,  however,  does  not  lay 
at  the  apexes  of  the  domes  but  a  short  distance  below.  The  best  gas 
and  oil  wells  on  the  dome  in  Petty  township,  Lawrence  county,  are  from 
50  to  100  feet  lower  than  the  apex.  The  smaller  domes  in  Lawrence 
county  show  good  accumulations  of  oil. 

The  uppermost  part  of  the  flanks  of  the  major  fold  contain  abundant 
oil.  The  oil  decreases  in  quantity  toward  the  outer  boundaries  of  the 
field.  The  western  limit  is  abrupt  and  the  wells  along  this  boundary 
produce  abundant  water.  Enough  data  are  at  hand  to  conclude  that 
this  is  a  line  of  water  saturation  and  that  above  this  line  and  over  the 
fold  most  of  the  sands  are  wholly  oil-bearing.  The  Pottsville  rocks  are 
exceptional  in  that  they  contain  water  in  the  lower  portions   and  in 


144  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

some  cases  are  wholly  saturated  over  the  fold.  These  rocks  are  widely 
distributed  over  Illinois  and  are  conspicuous  for  their  yield  of  salt 
water.  The  sands  lower  than  the  Pottsville  and  the  upper  Bridgeport 
and  Eobinson  lenses  do  not  show  much  saturation  over  the  crest  of  the 
anticline.  There  are  one  or  two  spots  in  the  field  that  show  isolated 
patches  of  water-bearing  sand,  particularly  in  the  Kirkwood  and  Mc- 
Closky  sands. 

Some  of  the  non-producing  wells  in  the  producing  areas  owe  their 
condition  to  impervious  sands  or  thinning  out  of  producing  sands. 
Lack  of  porosity  will  perhaps  explain  the  position  of  dry  wells  often 
occurring  at  or  near  the  very  minor  domes  or  small  pits  that  occasion- 
ally exist  along  the  crest  of  the  fold. 

Prospective  Pools. 

It  is  probable  that  the  high  spots  along  the  crest  of  the  major  fold, 
especially  the  one  in  section  30,  Petty  township,  Lawrence  county, 
represents  cross  folding  or  buckling.  This  condition  would  suggest 
that  the  territory  east  of  the  fold  would  be  similarly  affected,  particu- 
larly in  the  lower  producing  formations.  New  pools  are  then  possible 
to  the  east  of  the  fold  in  positions  and  directions  perpendicular  to  the 
trend  of  the  field  and  parallel  to  the  raised  portions  of  the  anticline. 
The  presence  of  oil  in  Honey  Creek  and  Montgomery  townships  of 
Crawford  county  seem  to  bear  out  this  relation.  The  chief  raised  por- 
tions of  the  fold  occur  in  section  1,  the  northwest  corner  of  section  18, 
and  section  30  of  Petty  township;  sections  10  and  14,  Lawrence  town- 
ship and  sections  23,  26  and  35  Dennison  township,  all  of  Lawrence 
county. 

The  western  side  of  the  Crawford  and  Lawrence  county  oil  fields, 
with  one  exception,  is  sharply  defined  and  is  bounded  by  a  line  of  water 
saturation.  In  addition  to  this,  the  dip  of  the  strata  into  the  Illinois 
basin  is  so  pronounced  that  the  only  possibility  for  new  pools  lies  along 
unknown  terraces,  similar  to  the  one  occurring  in  section  29/  Bridgeport 
township. 

The  extension  of  the  south  end  of  the  field  is  problematical  and  al- 
most impossible  to  forecast  with  the  present  development,  owing  to  the 
lack  of  data  and  the  uncertain  character  of  the  anticline.  It  is  also 
likely  that  the  gap  between  the  Lawrence  and  Crawford  county  fields 
will  remain  barren  as  it  seems  to  represent  a  large  transverse  basin  on 
the  fold. 

Possibilities  for  the  production  of  oil  in  sands  in  Crawford  county, 
corresponding  to  the  deep  producing  formations  of  Lawrence  county, 
are  slight  because  of  the  established  fact  that  these  formations  grad- 
ually pinch  out  to  the  north  of  Lawrence  county. 


blatchley]         ECONOMIC    FEATURES    OF    THE    ILLINOIS    FIELDS.  145 


CHAPTER   VI. 


Economic  Features  of  the  Illinois  Fields. 


INTRODUCTION. 

The  discovery  of  profitable  quantities  of  oil  in  Clark  count}'  in  1904 
and  1905  led  to  a  remarkably  rapid  development  of  the  oil  fields  in  the 
State.  The  development  is  all  the  more  surprising  when  it  is  noted 
that  in  the  short  period  of  six  years  a  production  of  such  proportions 
reached  its  zenith.  Other  great  fields  of  America  required  as  high  as 
30  years  to  attain  such  a  position.  Besides,  the  Illinois  production  comes 
from  the  smallest  areal  extent  of  oil  producing  territory  of  the  first 
seven  ranking  states : 

Square  miles  of 
Rank.  State.  petroleum 

lands. 

1  California  850 

2  Oklahoma  400 

3  Illinois  250 

4  West  Virginia  570 

5  Ohio  650 

6  Texas  400 

7  Pennsylvania  2,000 

Illinois  gained  ninth  place  for  production  and  value  of  oil  in  1906 
and  third  place  for  both  in  1907.  Since  1907  the  State  has  held  third 
place  for  production  and  second  for  value  and  has  been  exceeded  only 
by  California  and  Oklahoma.  Up  to  January  1,  1912,  about  19,982 
wells  had  been  drilled  for  oil  and  gas  in  the  State,  of  which  15.7  per 
cent  were  barren.  The  remaining  84.3  per  cent  have  produced  since 
1905  about  157,905,084  barrels  of  oil,  valued  at  about  $101,666,473. 
The  extent  of  the  fields,  the  grade  of  the  oil,  and  the  efficiency  of  pro- 
duction, place  them  among  the  greatest  of  the  world  from  an  economic 
point  of  view. 

The  successful  growth  of  the  Illinois  fields  may  be  attributed  par- 
ticularly to  the  quiet  efficiency  of  experienced  and  capable  oil  men.  The 
Appalachian  fields  supplied  the  greatest  influx  of  operators,  and  these, 
through  many  years  of  training,  determined  the  trend  of  development. 
They  soon  established  the  limits  of  the  field  and  thus  prevented  useless 
explorations. 

—10  G 


146  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

After  oil  has  been  found  in  commercial  quantities  in  the  shallow  Casey 
pool,  the  operators  began  to  drill  in  all  directions.  They  were,  however, 
soon  limited  east  and  west  of  Casey  by  boundaries  which  were  defined 
by  barren  wells  that  either  failed  to  show  oil  or  yielded  large  quantities 
of  salt  water.  This  caused  a  shifting  of  the  development  inward  and 
along  a  north  and  south  direction.  The  discovery  of  oil  in  deeper  sands 
in  Crawford  county  led  to  the  same  tactics  of  development,  and 
eventually  the  long  narrow  strip  of  oil  country  in  Clark  county  ap- 
proached the  broader  pool  of  Crawford  county.  Similarly,  the  move- 
ment continued  from  the  deeper  productive  fields  of  Lawrence  county. 

The  Illinois  fields  are  somewhat  different  from  others  because  of 
local  conditions  and  the  necessity  of  properly  and  economically  caring 
for  enormous  quantities  of  oil.  The  business  is  divided  into  many 
branches,  each  of  which,  from  the  first  step  of  leasing  to  that  of  an 
established  production,  requires  careful  and  systematic  attention.  The 
Ohio  Oil  Company  (Standard)  controls  most  of  the  production  and 
under  its  management,  there  have  sprung  up  various  departments  neces- 
sary to  cope  with  the  rapidly  increasing  yield  of  oil.  This  has  been 
done  remarkably  well  and  as  has  been  truthfully  said,  "there  never  has 
been  an  oil  field  so  well  taken  care  of  in  so  short  a  time  as  that  of 
Illinois." 

The  following  general  discussion  of  the  several  phases  of  the  oil 
business  is  made  with  a  view  of  enlightening  those  readers  who  are  not 
familiar  with  the  business.  It  is  not  intended  to  be  an  authoritative 
explanation  of  the  methods  used  in  developing  an  oil  field  or  of  the 
details  of  drilling  a  well. 


DEVELOPMENT  OF  OIL  PEOPERTIES. 

FORENOTE. 

The  first  step  necessary  to  the  development  of  any  oil  field  is  a  busi- 
ness-like lease  of  the  land,  conveying  distinct  rights  to  both  the  land- 
owner and  the  lessee.  The  successive  steps  of  choosing  well  sites, 
drilling,  shooting  wells,  and  equipping  oil  properties  involve  activities 
separate  from  each  other,  yet  so  connected  that  each  is  a  necessary  part 
of  the  whole.  In  fact,  the  largest  oil  companies  in  Illinois  have  separate 
branches  for  leasing,  drilling,  buying,  pipe-line  discharging,  telegraph- 
ing, and  engineering. 

The  first  step  of  the  oil  operator  after  learning  of  an  "oil  strike,"  is 
to  lease  as  near  as  possible  to  the  producing  wells.  If  he  has  sufficient 
knowledge  of  the  geological  structure  of  the  area,  he  follows  the  trend 
of  the  anticline  or  terrace,  as  the  case  may  be.  If  he  feels  that  his 
properties  are  within  the  limits  of  possible  producing  territory,  he  makes 
his  locations  and  starts  his  drilling. 

It  is  regrettable  that  many  inexperienced  operators  are  attracted  by 
the  rush  to  newly  proven  areas  and  by  lack  of  knowledge  of  both  the 
nature  of  the  business  and  underground  conditions,  are  led  to  failure. 
It  is  often  the  case  that  such  novices  open  up  a  field.  Any  observer  of 
the  oil  business  will  soon  note,  however,  that  the  larger  companies  and 
operators  do  but  little  "wildcatting,"  preferring  to  profit  by  the  ex- 


ILLINOIS    STATE    GEOLOGICAL    SURVEY. 


Bull.    No.    22,    Plate   XVI. 


The   standard  derrick. 


blatchley]  LEASING  OF  OIL  PROPERTIES.  147 

perience  of  the  novice.    It  is  true  also,  that  field  limits  of  many  proven 
areas  are  established  only  by  these  indiscriminate  test  holes. 

Leasing. 

In  contrast  with  the  oil  territories  of  the  mountainous  Appalachian 
regions  and  of  the  far  west,  Illinois  is  a  drift-covered  plain.  All  of  it 
is  either  in  cultivation  or  devoted  to  pasture.  The  land  divisions  are 
simple  and  uniform  and  are  based  on  the  civil  township  of  thirty-six 
sections.  Each  section  usually  is  sub-divided  into  tracts  of  the  mul- 
tiple of  twenty  acres.  The  leasing  of  properties  then  starts  upon  a 
simple  basis. 

There  are  no  set  rules  concerning  leasing  as  this  is  necessarily  de- 
pendent upon  local  conditions.  The  oil  men  deal  entirely  with  in- 
dividual land-owners,  and  leases  are  private  bargains.  While  some  of 
the  territory  is  developed  by  land-owners,  it  is  more  often  leased  to 
operators  for  a  period  of  five  years,  with  option  of  further  lease  as  pro- 
duction continues.  If  adjoining  property  is  untested  at  the  time  of 
leasing,  the  farmer  usually  receives  a  royalty  of  from  one-eighth  to  one- 
sixth  of  the  future  production,  with  the  further  stipulation  that  drilling 
is  to  begin  within  six  months  to  two  years,  or  that  a  stated  rental  per 
acre  will  be  paid  until  the  first  well  is  drilled.  If,  on  the  other  hand, 
the  desired  property  lies  near  producing  territory,  the  land  assumes 
added  value  and  a  bonus  is  demanded  in  addition  to  the  royalty  and  the 
reservation  of  the  fee.  The  closer  the  farm  is  to  good  oil  properties,  the 
higher  the  bonus  becomes;  it  averages  from  $10.00  to  $40.00  per  acre, 
but  sometimes  reaches  $200.00  or  more  per  acre. 

The  land-owner  retains  all  surface  rights  of  the  land,  except  on  the 
portion  necessarily  used  by  the  operator  for  his  equipment,  including 
a  full  quota  of  wells,  power  house,  boiler  house,  tankage,  waste  pit,  and 
pull  rods.  Upon  an  80-acre  tract  not  more  than  six  acres  are  necessary 
for  this.  A  large  portion  of  the  land  in  the  oil  district  is  not  con- 
sidered especially  valuable  from  an  agricultural  point  of  view  and  con- 
sequently but  little  restriction  is  placed  upon  the  operations. 

In  certain  portions  of  the  field,  industrious  farmers  till  their  ground 
and  at  the  same  time  derive  a  good  income  from  oil.  If  a  large  storage 
of  oil  is  contemplated  it  is  customary  to  buy  the  land  outright  for  a 
so-called  tank-farm. 

Stipulations  are  usually  made  regarding  the  use  of  gas  by  the  land- 
owner and  of  payment  by  the  lessor  for  active  gas  wells.  This  generally 
averages  from  $i 00.00  to  $200.00  per  well  per  year.  There  are  but  few 
large  gas  wells  in  the  Illinois  fields  and  the  income  is  insignificant  as 
compared  with  that  derived  from  the  vast  production  of  oil. 

The  lessee  further  agrees  not  to  drill  wells  closer  than  200  feet  to 
any  dwelling  or  barn,  except  in  the  case  of  town  lots.  (See  PL  XXIII, 
B.)  This  may  be  made  optional  with  the  land-owner  and  merely  serves 
as  a  protection  to  his  perishable  property. 

It  is  also  agreed  that  the  lessee  shall  be  responsible  for  all  damages 
caused  to  growing  crops,  provided  there  is  enough  in  amount  to  warrant 
complaint.  Oftentimes  when  a  well  is  shot  and  a  good  flow  is  secured, 
the  wind  will  spray  the  oil  over  a  considerable  area  of  growing  grain 


148  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

and  will  thus  render  it  unfit  for  use.  Again  careless  driving  over  culti- 
vated ground  will  destroy  a  portion  of  the  crop  and  so  warrant  com- 
plaint.    All  pipe  lines  are  buried  below  plow  depth. 

After  production  is  established,  the  lease  becomes  the  most  valuable 
part  of  the  oil  property.  It  is  often  sold,  the  price  depending  mainly  on 
the  number  of  producing  wells  and  their  average  daily  yield.  A  trans- 
fer of  lease  often  takes  place  even  though  no  wells  have  been  drilled  on 
the  tract.  The  price  of  this  is  dependent  upon  the  distance  from  proven 
property.  In  fact,  lease  speculation  has  become  a  very  lucrative  busi- 
ness, particularly  in  newly  opened  areas.  The  speculator  watches  the 
prospecting  and  upon  the  first  news  of  the  oil  strike,  rushes  to  the 
locality  and  leases  what  he  can  without  a  great  amount  of  expense.  The 
demand  for  land  "close  up"  to  the  active  wells  soon  outstrips  the  supply 
and  the  unfortunate  operator  who  is  late  or  who  really  wishes  to  drill, 
is  forced  to  pay  the  speculator's  price.  A  good  example  of  this  type  of 
traffic  was  shown  in  the  recent  Carlyle,  Illinois  excitement. 

The  following  form  of  lease  is  in  common  use  in  Illinois : 


ILLINOIS   STATE  GEOLOGICAL   SURVEY.  Bull.   No.    22,  Plate  XVII. 


The   steel  derrick. 


BLATCHLET] 


LEASING  OF  OIL  PROPERTIES. 


149 


B  £2  «"2  i 

-^  J2  ,C  w  3  rj 


'.  X 


•  o 


Eg  •  :  : 

<u  ©   ■   •   « 

££  :  :  : 

cd+j    . 
<u  ®  .   • 

b-°   •   '   * 

so    :  "j 
^2  *  :S 

3    -<t-i  ra 
d    •  O  ft 


of 


g« 


O-M 


-OS'S 


S-d 


fa"~ 
£be.§ 


3  fa- 

oj  a>  h 

3      ^  w  3      ' 

fa  _,  *C  O)  TO   ,„ 


.5  o  w       c  3  cj 

O        +J  _*   fa   fa  Mi 
<D        2^  ft 

eflws  d 

3>>&do^£ 

O  £  £        3  g  g 

-m  2  3  w  ^  <y 
S*  o  «j£ 

3  02        5c* 
ft       d"*   O^ 

<G  f»j+j  _,  co  +-> 
cd      o  a)  a)  _r 

«,  ft  aid        fa 

>>3  3+3+-> 

q   3  03 
3«-«  fa  fa  w 
£  £  be  O  cj 

£     •  ft+J 


3^d 


^  fa   -  ^  d 

.  3  o+3.£  3 
•+j  ft      cH 


,C3  j 

•d 

.     y  KM 

•  a)  H 

'  M  H 

!  05  M 

..3  X 

■■*  e 


,  o  rf  3  3 
.  >       ft  ^2 

!U    ftrQ«H 

c 


©■ 


d  a) 


<H 

ft"^ 

'  _ 

o 

02 

•3 

■Ooj° 

5^ 

0) 

g 

0) 

■   X 

d" 

4-> 

ft 

•^ 

O) 

.0) 

ft 

•  3 

13 

o3>d 

P3 

;t) 

O 

_.  CO 

•a 

>. 

gjj 

Cod 

fa 

O  to 

~d  - 

^ 

O  CO 

-  •/. 

o 

v.  — 

<H 

LJ      U 

od 

O  3d 

bed 


^2  Oj 

0)'+-! 


■"2 

o2 


CD  Oj 


•m  O-O  >>^  3 

«  o  §  » 1  2 

"^  o  W  3  bC 
■^.S*--  co  cj  w 
oftg  ."g  CJ 
4->  <d^3  2.3 
O)  5:  o  3+3 

OJ 

^9 


aj+j 


S  3d  c, 
a>—  cj  3 


o  o  cj^^  ^ 

«m  cd  cd  cp  «M 
...0,15  beg  cd 

"^S"^  ®  H   Si 

••   -  fa  fa>d 

<U  3      &  3-? 

fa'.Efd^co' 

bCS^cdw-CJ 


33^ 


*j  3 
.5  ft 

.  *d 


•.S3 


3  u 

OS  ^ 


£5 


£°d 

3     CD 
m   ft    W 


^  ft  .fa"  CD     CJ 

+J  CD  *&A   A 


t?-^     fa  w     •*? 

■3b  cj  a)  -ri 

•  ^ft^'-S  s 
•3     cjr  & 

•  o  fa  .3  3 

•  •  -  a,   +^  cd   d 

•  CD  ,q     O  .3    £ 

:1l-ftx 
•  Sa  3ch 


rf       d  CJ  J  3 
„   02    C   ft  fa   ft 

E^ei       ft 
ti  -r  ro  02  ^  CD 
3CJ       fa^^ 
3  —  d  3  £ 
3     •  0)35  n 
QJ 

^3 

CD 

•  b  ^ 

■  co  a> 

:3c3 


■3  S 

S2 


+33 

'  !W  M     -  — I 

'•"3  ^ 


fa 

w 

o 
3 


d^=      "- 

—    !U 


3 

fa  3 

v-  (-  02     CD 

6pS  bC   CD 


•ftS 


'o   ■  "ca   ■   o  02^ 
sg.SSg^fa0 

<S  ft  o  *s? 
fa  3  9.02  3  o  5 
2^       3-m  o  3Q  C 

>02023+J02M3 
0   3         3  CJ 

cj  3   «-<   !  H 

3  CO         r*   r-1  fa-      •  r- 

S  be  be  OS'S   .  g 

c  °  fa^    •  3 

<«  Ofa-;     3*2   •  5 

-Z-z^S  :§ 

02^  ^bd  'CD 

cjfH^Q.C'H  :  ,3 

boo         <ri  o    .+-> 

02  e  •"  d       fa      +j 

ft+^  03   •-»-' 

fa  3d  CJ  fa  CD     • 

3  jr;  oj  72  3  +^    •  d 

02  aJd      <fa  3    •  cd 
d-^         d    '  cj 

3  02  w  w  g    •  -rt 

ioTs^  ' 

^  §  2  be  £ 
d.S  ft     o 

2^3° 
beS"^  ©  ^ 

3    s5*-1.^; 

'-^3  3  +j 
.60  O  «w  §  CD 
^   fa   02   S   CD 

3  ^  M  3  +^ 
3+3^  ft 
-d      ^ 


;ft5 
:d6 


w  3 

CD 

■  d^; 

,  CD  fa 

•33  3 


■d 

■  cd  be 

:§■§ 


3  "3  bo+3  cd 

CD  2  ■ 

^  3 


3>> 


02 

^   o        +J  O 
02  .,  CD +3 

fa  •-  be  cd  — ' 

3  -3  3  02  ^ 


7. 


w  bo  3  >>  3 

6  a  'H    « 

•^  +j  O  -a  fa 

CD  .CJ 

3  ^ 

fti^CD 

3_  >      -3 
P  3  g.S  o 


3  fa  CD 


O 
02° 

-3  - 


C  3 
3  o 


ft^H 

3 

fa  3 
O  O 


dd 


fa  3  3  O        c  3 

3    ^S*3fal»^  . 

^^ft-2-S 

>jd  >-j  02      o^  h"-;  3 

as S'g^     »  § 

0  P  yj  ifa-2.2  3^d 


awrtS8iia>jj-s 


d  O' 


3  3 


g^|oo5^  ft2gc32:.2>> 

r->       "^Hil'r'CDJ_>+JCDfa         n  +J  fa 

^cd^     -^M/J£f^2 
ofa*0  ^CJ  ^+3o.-  -r«>^3ajSS>fa 

O  ^    (13    t-H  t-l         _C  d   m    m  -h    W    g  .rn 


:fe'3  "6 
'.Q 


ss« 


^  ■»  CD   CD  '3  £  "3  K   bjj  2   O  3 


150 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


03  03 
o 


ft 

Sh  cu 
3  O 


co  S 


o3^ 


ja  .2 

d   +-> 


A 

72 

O4 

c 

o 

XI 

a 

c3 

•V 

03 
Pi 

O 

fii 

« 

a 

2 

<p 

>d 

>, 

xi 

b/j 

a 

>d 

£  2 

ft  o 

>  m 

o  o 


C     73 

s  03 
be 

03    ctf 

.&  s 

ft  a3 

C3 
£>> 
X2    ft 

o  o 


0)     0) 

bo  bD 


ft  ft 
d  "d 

c  S 
o   o 


ft^S^03 
o  StJ.2  S 

IN*- 

+-1   C  „  ,   TO   03 

boSa>gco 

£   >,+■'"  03 
°   C  •>.!»   C 


~  3  s-  5 

S      ^+->  "   03 

■s  :so3 

*S3  "  53  o 

3«CX« 

o    S 


03-£         oj 
0J   03   C        .•£ 


^ftW03 

03   3        t^5 


-^^X 


S£^i 


^  r  3  o^d 


►J,dd+->  03 

C  n  w  ft  o 

0        -      2 
o    „  wd  d 

CU   73   03 -h 
73^   03    c3   O 

X   f>  CU+J   73 

■<->  rlrlO) 

p  ftcd^ 
*o      »X3 


bo-*5 


cd 


+j  ft 
5°^ 


cu 


03.27  d 
Jh   73     c 

03    73    5 

d+->  c 
o  &  be 

3^-s 

7;  73 

d-s  .S 


H^^^^d 
gftSo-cl 

73C  ftcS^ 


J 

J 

J 

■•'  <J 

3 

<j 

W     H 

H 

H 

CC      CO 

to 

CO 

O     03 
73     rn 


73 


is » s 

3     03      £ 

03 
X) 


ILLINOIS   STATE   GEOLOGICAL   SURVEY 


Bull.  No.   22,  Plate  XVIII. 


B. 


A  nitroglycerine    plant. 

A    storage    magazine    for    nitroglycerine. 


blatchley]  DRILLING   OF   OIL   WELLS.  151 

Choosing  a  Well  Site. 

When  the  lease  is  secured  and  the  operator  is  ready  to  drill,  he  must 
choose  the  site  for  his  first  well.  This  is  governed  by  one  or  two 
generally  recognized  rules  or  courtesies  and  many  local  circumstances. 
It  is  usually  the  custom  to  place  wells  about  210  feet  inside  the  property 
line.  This  varies,  however,  with  different  depths  of  sand.  Wells  in  the 
shallow  fields  are  often  placed  100  feet,  or  perhaps  less,  from  the 
property  lines.  The  drilling  is  usually  inexpensive  and  many  wells  are 
drilled  in  the  eager  demand  for  the  oil,  with  the  result  that  such  a 
field  is  quickly  drained.  The  location  lines  in  Crawford  county  are 
almost  always  maintained  at  the  regular  interval  of  210  feet  from  the 
line  but  in  the  deep  Lawrence  county  pools  the  distance  is  from  250 
to  300  feet.  The  distance  between  wells  on  the  same  lease  depends  on 
expense  and  other  factors.  In  the  Clark  and  Crawford  county  fields 
they  are  generally  placed  450  feet  apart,  but  in  Lawrence  county,  wells 
to  the  deeper  sands  are  located  660  feet  apart. 

An  unwritten  law  among  operators  in  most  fields  requires  the  lessee 
to  drill  opposite  producing  wells  on  adjoining  property.  This  is  called 
"offsetting"  and  is  done  to  protect  property  lines  and  prevent  drainage 
of  oil  from  the  lease.  It  has  been  legally  determined  that  a  landowner 
can  bring  suit  to  make  a  lessee  "offset"  wells  or  else  secure  the  surrender 
of  the  lease.  It  is  the  custom  to  offset  all  adjoining  wells  on  the  neigh- 
boring leases  and  leave  the  centers  to  be  drawn  upon.  The  free  space 
in  an  80-acre  tract  thus  measures  900  by  2,250  feet.  The  line  wells 
then  draw  to  good  advantage,  and  unnecessary  center  wells  are  avoided. 
It  is  a  difficult  matter  to  estimate  the  acreage  drawn  upon  by  oil  wells. 
This  is  dependent  upon  the  thickness  and  porosity  of  the  sand,  the  area 
of  the  pool,  and  the  location  distances  of  the  wells.  It  is  estimated  that 
about  five  acres  are  drawn  upon  by  the  Clark  county  wells,  eight  in 
Crawford  county,  and  ten  to  twelve  in  Lawrence  county.  Without  con- 
sidering center  wells,  twelve  to  fourteen  are  drilled  on  an  80-acre  tract 
in  Clark  and  Crawford  counties  and  from  eight  to  ten  in  the  Lawrence 
county  field. 

The  choosing  of  a  site  may  be  affected,  furthermore,  by  sudden  dips 
in  the  sand  about  a  regular  location,  thus  breaking  up  the  regularity 
of  location  lines.  Further  irregularity  may  be  caused  by  the  presence 
of  buildings,  permanent  power  houses,  or  unfavorable  topographic  fea- 
tures. It  may  seem  advisable  to  even  shift  wells  from  a  drift  covered 
valley  to  the  side  of  a  hill  where  less  expense  is  incurred  in  placing  the 
drive-pipe.  Well  locations  are  often  chosen  in  prospective  areas  with 
respect  to  the  water  and  fuel  supply.  The  advance  of  oil  operators  into 
active  coal  fields  of  the  State  may  necessitate  selection  of  well  sites  so 
as  not  to  endanger  mines  and  their  employees. 

Drilling. 

The  third  step  in  the  development  of  oil  properties  is  a  contract  be- 
tween the  operator  and  the  drilling  contractor.  An  agreement  is  drawn 
up  between  the  two  for  the  drilling  at  a  certain  price  per  foot,  dependent 
upon  the  locality  and  the  depth  of  the  desired  sand.  A  uniform  rate 
is  usually  established  by  the  supply  houses  in  an  active  oil  field.   Drilling 


152  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

in  "wildcat"  areas  usually  costs  more  than  in  a  proven  area  because  of 
the  distance  from  railroads  and  the  lack  of  material,  fuel,  water,  etc. 
Deep  sands  and  peculiar  formations  also  affect  the  cost  per  foot  of 
drilling. 

Stipulations  are  made  in  the  contract  for  drilling  a  specified  depth 
and  the  contractor  is  held  responsible  for  the  well  to  that  depth,  or 
possibly  to  the  extent  of  reaching  the  desired  sand  and  determining  its 
productivity.  The  agreement  states  that  drilling  shall  begin  within  a 
specified  time. 

The  contractor  is  responsible  for  the  purchase  and  construction  of 
the  derrick.  He  furnishes  boiler,  string  of  tools,  fuel,  water,  drillers- 
and  tool-dressers,  and  is  held  responsible  for  accidents.  The  contractor 
must  replace  the  casing  after  a  successful  shot;  clean  out  the  well  and 
pump  it  for  a  specified  time  free  of  charge,  and  tube  the  well.  Should 
further  cleaning  be  necessary  after  the  time  stated,  a  charge  is  usually 
made  by  the  contractor  for  this  service  at  the  rate  of  $15.00  per  day 
and  the  operator  furnishes  fuel  and  water.  A  rate  of  $2.50  per  day  is 
usually  made  for  extra  pumping.  The  contractor  is  permitted  to  use 
any  oil  or  gas  as  fuel  for  drilling  that  he  may  find  during  the  progress 
of  his  well.  If  the  contractor  experiences  trouble  in  setting  his  casing, 
he  is  usually  paid  a  reasonable  amount  for  labor.  In  case  a  dry  hole 
is  secured  the  contractor  must  pull  all  the  casing  possible  and  in  the 
event  of  a  producing  well  he  must  draw  that  casing  which  is  not  desired 
in  the  well.  In  all  events  the  contractor  must  put  the  well  in  order 
for  pumping. 

The  operator,  on  his  part,  usually  agrees  to  furnish  conductor,  drive- 
pipe,  casing,  tubing,  and  rodding.  He  provides  for  hauling  the  pipe 
and  necessary  accessories  other  than  the  driller?s  string  of  tools  and 
rig.  The  operator  is  responsible  for  the  plugging  of  a  dry  well  and  the 
filing  of  the  affidavit  thereto. 

When  the  contract  for  drilling  is  signed,  the  operations  pass  into 
the  hands  of  the  contractor,  who  in  turn  contracts  with  the  rig-builder. 
Nearly  all  rigs  in  the  Illinois  fields,  outside  of  the  Clark  county  pools 
and  portions  of  Crawford  county,  are  of  the  Standard  type.  (See  PI. 
XVI.)  They  are  constructed  of  timber  and  consist  of  four  strong  up- 
rights held  in  the  shape  of  a  pyramid  by  ties  and  braces,  and  resting 
on  strong  wooden  sills.  This  derrick  is  used  as  a  support  for  the  sheave 
or  crown  pulley,  which  must  be  of  sufficient  height — 66  feet  in  the 
shallow  fields  and  72  feet  in  the  deeper  fields — to  swing  the  long,  heavy, 
drilling  tools  free  from  the  derrick  floor.  A  second  pulley  is  fastened 
to  the  top  to  swing  the  bailer  free. 

Connected  with  the  derrick  are  principally  the  bull-wheel  and  shaft 
on  which  is  wound  the  cable  supporting  the  drilling  bit;  the  walking 
beam,  giving  vertical  motion  to  the  tools ;  the  band  wheels,  transmitting 
power  from  the  engine  to  the  movable  parts;  and  the  sheds  to  protect 
the  engine,  bull-wheel,  and  shaft  from  inclement  weather.  When  these 
main  portions  of  the  derrick  with  necessary  minor  details  are  complete, 
the  rigbuilder  has  fulfilled  his  part  of  the  contract.  The  contractor 
then  sets  his  boiler  in  place,  adjusts  his  engine ;  winds  his  cables ;  places 
his  swinging  cranes  for  lifting  the  drilling  bits;  and  does  many  trivial 
things  necessary  to  facilitate  his  work. 


ILLINOIS    STATE    GEOLOGICAL   SURVEY. 


Bull.    No.    22,    Plate   XIX. 


... 

^1*  ..JjB  ^^BS^frw,  '    '  ,g^«»**^-? 

pbx 

^  M 

-"  jpr   '^~!55*il1' '— ^  ^        ^ 

- 

- 

WHS           -.   «ar  HP          <w** 

. ,.  -  r^" 

:r_ 



Oil    tanks    under    shed. 
A   pumping   disc. 


BLATCHLET]  DRILLING    OF    OIL   WELLS.  153 

The  construction  of  the  standard  rig  requires  about  three  days  and 
costs  about  $500.00.  The  same  derrick  can  be  used  about  twelve  times, 
at  an  extra  cost  of  about  $100.00  each  time  for  tearing  down  and  re- 
building and  for  additional  repairs  and  materials. 

The  steel  derrick  (see  Plate  XVII)  is  used  in  some  portions  of  the 
field,  though  not  extensively.  The  uprights  are  of  steel  and  the  braces 
and  ties  are  of  wire,  cable  or  thin  steel  rods.  The  sheds,  shaft,  and 
bull-wheels  are  of  wood.  The  steel  derrick  can  be  torn  down  easily  and 
moved  indefinitely  but  its  original  expense  is  much  greater  than  the 
standard  derrick.  The  leading  objection  to  the  steel  derrick  is  the 
probability  of  breaking  or  twisting  pieces  of  the  frame  work  during 
transportation  and  causing  delay  in  expense  and  repair. 

In  the  shallow  fields  a  portable  drilling  rig  is  more  often  used  than  a 
permanent  one.  The  whole  outfit  is  mounted  on  a  heavy  wagon  and 
includes  a  single  high  timber,  fitted  up  as  a  derrick,  while  the  remain- 
ing necessary  parts  are  assembled  in  a  compact  manner  back  of  it. 
This  rig  is  not  practical  for  deep  sands  or  hard  formations.  There 
are  two  types  of  portable  rigs,  known  as  the  "Star"  and  the  "Parkers- 
burg."  Their  cost,  including  all  equipment,  is  about  $2,300.00.  A 
larger  type  of  portable  drilling  rig  has  been  perfected  recently  that  is 
suitable  for  deeper  sand  pools.     The  cost  of  this  rig  is  about  $10,000.00. 

The  costs  of  drilling  wells  in  Illinois  has  gradually  declined  since  the 
opening  of  the  Casey  field  in  1906.  At  that  time  the  cost  was  $1.00 
per  foot  when  fuel  and  water  were  not  included,  and  90  cents  per  foot 
when  they  were  supplied.  The  following  costs  of  drilling  are  represen- 
tative for  the  various  pools : 

Cost  of  Drilling  in  Illinois  Oil  Fields. 

Pools.  Depth.  Cost  per  foot. 

Clark  county,  400  to  500  feet $0  80 

Crawford  county,  750  to  1,000  feet,  1907 1  00 

Crawford  county,  750  to  1,000  feec,  1908 0  90 

Crawford  county,  750  to  1,000  feet,  1909-1910 0  80 

Crawford   county,   750   to   1,000   feet,    1911 0  70  to  0  85 

Lawrence  County — 

Bridgeport   sands,    800   to    950   feet,   with    10-inch    drive-pipe 

and    6    5/8-inch    casing 0  80 

Bridgeport    sands,    with     16-inch     drive-pipe     and     8%-inch 

casing     1  35 

Buchanan  sands,  1,250  to  1,400  feet 1  35 

Kirkwood  sands,  1,450  to  1,650  feet 1  50 

Tracey  sands,   1,700   to   1,750  feet 1  50 

McClosky  sands,  1,775  to  1,875  feet 1  50 

The   approximate   time   required  to   drill,   shoot,   clean,   and  put   in 

order  a  well  in  the  different  pools  is  as  follows : 

Pool.  Days. 

Clark  county,   or   Shallow   sands 4  to     5 

Crawford    county    10  to  12 

Lawrence  County — 

Bridgeport    sands    10  to  12 

Buchanan  sand    20  to  25 

Kirkwood  sand   35  to  45 

Tracey  sand    60  to  75 

McClosky  sand 60  to  100 


154  OIL  FIELDS  OF  CEAWFOBD  AND  LAWEENCE  COUNTIES,   [bull.  no.  22 

The  Bridgeport  sands  were  the  first  developed  in  Lawrence  county 
and  were  drilled  with  the  small  sized  pipe  similar  to  that  used  in  the 
Eobinson  sand  of  Crawford  county  which  is  at  the  same  depth.  Later 
when  the  deeper  sands  were  discovered  and  found  more  prolific,  it  be- 
came impracticable  to  use  6 14  inch  casing.  To  secure  production  from 
all  sands,  therefore,  a  larger  size  drive-pipe  and  8V4  inch  casing  were 
introduced.  The  operators  found  it  profitable  to  drill  new  wells  with 
larger  size  pipe  rather  than  redrill  the  older  ones.  The  old  wells  were 
allowed  to  produce  until  abandonment  and,  indeed,  there  are  many  that 
are  still  producing.     These  lie  close  to  the  town  of  Bridgeport. 

The  drilling  crew  consists  of  two  drillers  and  two  tool-dressers,  who 
work  by  pairs  in  shifts  or  "tours"  of  twelve  hours  each.  It  is  the  duty 
of  the  driller  to  stay  close  to  the  mouth  of  the  bore,  regulate  the  cable 
and  temper  screw  when  necessary,  control  the  machinery,  etc.  The 
tool-dresser  acts  as  an  assistant,  fires  the  boilers,  attends  to  the  engines, 
dresses  or  sharpens  the  bits,  assembles  the  small  tools,  switches  the 
bull-wheel  cable,  etc.  The  average  daily  wages  of  drillers  is  $5.00  and 
of  tool-dressers  $4.00. 

The  first  process  in  the  drilling  of  oil  well  is  that  of  "spudding" 
— a  method  used  in  drilling  the  first  75  to  150  feet  through  what  is 
known  as  the  drift,  and  usually  stopping  at  bed  rock.  The  drift  is 
composed  of  soil,  sub-soil,  clay,  gravels,  and  sands,  and  is  usually  soft. 
A  short  cable  is  fastened  by  a  shoe  to  the  crank  of  the  band  wheel  and 
to  the  general  cable  extending  from  the  bull-shaft  over  the  crown  pulley 
and  to  the  spudding  drill  in  the  well.  As  the  band  wheel  turns,  the 
short  cable  jerks  the  tools  up  and  down.  The  bull-shaft  is  clamped 
while  the  spudding  is  going  on  and  when  it  is  released  the  cable  and 
spudding  drill  are  fed  downward  into  the  hole. 

The  hole  is  usually  started  in  a  large  size  conductor  and  the  spudding 
apparatus  is  guided  by  hand.  The  regular  drilling  bit  and  stem  are 
too  long  and  heavy  to  manipulate  for  spudding. 

When  the  spudding  has  been  completed  the  stem  and  bit  are  sub- 
stituted and  are  connected  to  the  walking-beam  and  temper  screw  which 
lift  the  tools  and  cable  at  a  varying  rate  of  speed,  dependent  upon  the 
depth  of  the  well  and  the  condition  of  the  formations.  The  walking- 
beam  rocks  back  and  forth  on  an  upright  post  independent  of  the 
derrick  and  so  gives  vertical  motion  to  the  cable  and  drill.  The  temper 
screw  is  fastened  to  the  end  of  the  walking-beam.  The  cable  is  clamped 
to  the  lower  end  of  the  screw  and  as  it  is  necessary  to  lower  the  drill, 
a  handle  is  turned  and  the  tools  are  fed  downward.  The  driller  deter- 
mines the  lowering  of  the  cable  by  the  feel  of  the  rope  or  its  tension, 
and  the  temper  screw  is  adjusted  accordingly. 

The  temper  screw  varies  in  size  from  four  to  seven  feet,  the  average 
screw-depth  measuring  five  feet.  The  difference  in  length  is  due  to 
the  spring  of  the  hemp  cable.  After  a  screw-depth  of  drilling  has  been 
accomplished  the  tools  are  withdrawn  and  a  bailer  is  lowered  in  the 
hole.  The  bailer  or  sand  bucket  is  a  long  section  of  hollow  tubing  with 
a  ball  and  tongue  valve  at  the  bottom.  As  this  is  lowered  into  the  thin 
mud  and  liquid  at  the  bottom  of  the  well,  the  valve  opens  and  allows 
the  bailer  to  fill.    The  weight  of  the  liquid  closes  the  valve  as  the  bailer 


ILLINOIS    STATE    GEOLOGICAL    SURVEY. 


Bull.    No.    22,    Plate   XX. 


.Sjiiwli     ! 

HUHS^'V-' » *** 

V  ™    Mite  ***■  , ,  •  v  *\  f  ■  'i  w» 

.  »"  •▼A 

■  "~~--~    ^^»  -"^.v-    ---!_"  -•     „"           •    '"-  l/        < 

te 

B. 


A.  A   modern    tank-car   loading-   rack. 

B.  An    early   tank-car    loading    rack. 


blatchley]  SHOOTING  OIL  WELLS.  155 

is  lifted.     When  the  bailer  touches  the  ground  at  the  mouth  of  the 
well,  the  valve  releases  and  the  slush  pours  out. 

It  is  customary  to  place  drive-pipe  through  the  drift  to  bed  rock.  A 
square  hammer  is  usually  fitted  to  the  top  of  the  stem.  The  stem  rests 
inside  the  pipe  as.  the  hammer  strikes  the  top  of  it.  When  a  section  is 
driven  its  length  into  the  hole,  a  second  section  is  then  coupled  to  the 
first  and  the  driving  is  continued.  The  driving  of  the  pipe  is  manipu- 
lated with  the  same  apparatus  used  for  spudding.  The  first  casing  is 
usually  driven  through  the  first  salt  water  sand  and,  in  the  event  of  a 
bad  cave,  also  through  the  caved  material.  Casing  is  never  driven  until 
it  becomes  necessary  to  do  so.  In  case  the  driving  of  the  pipe  is  diffi- 
cult, a  sharp  heavy  shoe  is  attached  to  the  bottom. 


Shooting  the  Well. 

When  the  oil-bearing  stratum  has  been  tapped  and  found  productive 
the  work  is  continued  slowly  until  within  a  few  feet  of  the  bottom  of 
the  sand  or  until  evidence  of  salt  water  appears.  The  driller  notifies 
the  operator  who  in  turn  arranges  with  the  agent  of  a  nitroglycerine 
company  to  bring  the  explosive  and  shoot  the  well.  After  the  shooter 
has  measured  the  sand  accurately  with  a  steel-line  tape,  he  pours  the 
nitroglycerine  into  tin  shells  5%  inches  wide  by  5  feet  long,  holding 
from  10  to  20  quarts  each;  and  by  means  of  a  lowering  line,  pulley, 
and  special  releasing  device,  lowers  them  to  the  producing  sand.  The 
shells  are  conical  at  the  lower  end  and  concave  at  the  upper,  so  as  to 
fit  snugly  together.  The  top  shell  bears  a  water-proof  percussion  cap 
connected  by  a  wire  to  an  electric  hand-battery  above  ground.  A  "Jack- 
squib"  is  often  used  to  explode  the  shot.  This  is  a  tin  tube,  about  3 
feet  long  containing  a  dynamite  cap  packed  around  with  sand.  A  fuse 
is  extended  from  the  squib  and  is  lighted  and  lowered.  This  is  used 
when  the  hole  is  clean  and  not  caving  and  when  the  casing  is  not  pulled 
before  the  shot.  In  some  cases  the  squib  may  contain  a  small  quantity 
of  nitroglycerine  and  be  arranged  to  explode  with  a  time  fuse.  The 
explosion  opens  a  large  cavity  in  the  producing  sand  and  cracks  the 
bed  for  a  wide  radius,  thus  allowing  the  contained  oil  and  gas  to  flow 
to  the  well.  The  greatest  care  is  used  in  placing  the  shot  in  order  not 
to  disturb  the  overlying  shales  or  the  underlying  sand,  which  usually 
contains  salt  water.  If  the  shales  are  loosened  to  any  extent  they  fill 
the  cavity  with  debris  and  make  the  work  of  cleaning  the  well  difficult. 
In  case  it  is  known  that  the  lower  sand  does  not  contain  salt  water, 
drilling  is  carried  through  the  sand  and  a  pocket  is  made  by  the  ex- 
plosive to  catch  the  caving  material.  If  the  salt  water  sand  is  tapped, 
a  flow  is  often  started  that  is  difficult  to  control  and  which  often  drowns 
out  the  oil.  In  such  a  case  the  well  is  usually  abandoned,  although 
instances  are  known  where  the  salt  water  head  has  been  pumped  off  and 
a  production  of  oil  secured  later.  If  it  is  desired  to  shoot  the  sand  some 
distance  from  the  bottom,  an  anchor,  or  supporting  tube  for  the  shot  is 
placed  at  the  bottom  of  the  sand.  If  there  are  two  producing  sands 
close  together  two  charges  are  set  and  an  anchor,  loaded  with  nitro- 
glycerine,-is  placed  between  the  sands.  The  explosion  of  the  upper  shot 
transmits  the  force  to  the  second  through  the  anchor. 


156  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

The  size  of  the  shot  depends  upon  the  texture  and  thickness  of  the 
producing  sand. «  It  has  been  found  that  30  feet  of  sand  requires  about 
60  quarts  of  nitroglycerine.  A  charge  of  80  to  100  quarts  is  sufficient 
for  all  sands  in  the  Illinois  fields.  It  is  usually  the  custom  to  leave  the 
8  and  10-inch  casing  in  the  well  and  pull  the  casing  near  the  producing 
sand  previous  to  the  shooting.  This  eliminates  danger  of  collapsing  or 
mangling.     The  casing  is  lowered  later  in  cleaning  the  well. 

About  ten  seconds  after  the  shooter  has  discharged  the  explosive  there 
is  a  quick  jar  of  the  earth,  followed  by  a  muffled  report.  With  a  roar 
the  gas  pours  forth  from  the  well  in  a  bluish-white  streak,  followed, 
shortly,  by  a  column  of  oil  and  water.  This  rises  slowly  to  above  the 
top  of  the  derrick,  where  it  sprays  out  in  the  direction  of  the  wind. 
The  rattling  pebbles  against  the  derrick,  and  the  heavier  thuds  of  large 
fragments  on  the  ground  are  heard  for  several  minutes.  The  column 
of  oil  subsides  in  a  short  time  and  the  drillers  cap  the  well  or  turn  the 
flow  into  emergency  tanks. 

The  shooters  hold  responsible  positions  and  are  chosen  by  the  ex- 
plosive manufacturers  for  their  cool-headedness  and  skill.  They  re- 
ceive salaries  from  $100  to  $125  per  month  and  usually  a  bonus  for 
successful  work  and  good  behavior. 

The  torpedo  company,  through  its  shooter,  is  held  responsible  for  the 
well  from  the  moment  of  taking  charge,  and,  if  a  premature  shot  takes 
place  through  carelessness  or  neglect,  must  arrange  to  drill  another 
well  immediately  near  the  same  location  or  pay  for  the  ruined  well. 
When  the  shot  is  successful  the  contractor  resumes  charge  of  the  well 
and  completes  it  by  cleaning  out  and  putting  it  in  order  for  pumping. 
In  all  cases  the  shooter  is  required  to  know  that  the  well  is  in  perfect 
condition  before  shooting.  It  often  occurs  that  after  his  explosive  is 
partially  set,  the  overlying  formations  cave  and  cover  the  shot.  The 
shooter  and  drillers  cooperate  and  clean  out  the  well  very  cautiously  to 
the  top  of  the  shot.  Several  days  of  the  shooters  time  are  thus  re- 
quired before  he  can  complete  his  task,  at  an  extra  cost  to  the  company. 

The  torpedo  companies  maintain  manufacturing  plants  in  isolated 
spots  in  each  main  field  (see  PL  XVIII,  A).  Small  storage  magazines 
are  built  in  other  out-of-the-way  places,  usually  one-half  mile  from  any 
dwelling,  so  as  to  distribute  the  supply  and  avoid  large  loss  in  case  of 
accident  (see  PL  XVIII,  B). 

Special  transportation  is  necessary  to  distribute  the  nitroglycerine. 
Large  stock  wagons  supply  the  magazines  and  lighter  wagons  make 
distribution  to  the  wells.  The  nitroglycerine  wagon  is  built  on  strong 
but  flexible  springs,  and  is  easily  recognizable  because  of  the  height  of 
the  bed  above  ground.  The  bed  of  the  wagon  is  fitted  with  square 
padded  cells  for  each  10-quart  can  of  liquid.  The  words  "Nitrogly- 
cerine, Dangerous,"  are  printed  on  the  outside  of  each  wagon  and  serve 
to  notify  the  public  of  the  nature  of  the  vehicle.  The  shooter  usually 
drives  along  unconcerned  over  bumps  and  ruts,  confident  of  the  security 
of  his  peculiar  wagon.  Accidents  are  rare,  but  they,  sometimes,  may  be 
caused  by  collision  or  carelessness  in  pouring  the  liquid  into  the  cans. 
A  drop  on  the  side  of  a  can  may  be  exploded  by  friction.  The  viscous 
liquid  is  safely  poured  by  a  steady  hand. 


ILLINOIS    STATE    GEOLOGICAL    SURVEY. 


Bull.    No.    22,    Plate    XXI. 


A.  A    power    or    pumping    house. 

B.  A  boiler  house. 


blatchlet]  SHOOTING  OIL  WELLS.  157 

Both  liquid  and  solid  nitroglycerine  have  been  used  in  the  field. 
The  liquid  explosive  is  a  definite  chemical  compound,  known  as  tri- 
nitro-cellulose.  Glycerine  is  treated  with  a  mixture  of  concentrated 
sulphuric  and  nitric  acids  at  a  temperature  below  30°  centigrade  to 
prevent  explosion.  During  the  nitrating  process  water  is  given  off  and 
is  absorbed  by  the  sulphuric  acid.  The  temperature  of  30°  centigrade 
is  kept  uniform  and  is  effected  by  blown  air  during  the  mixing.  The 
rate  of  mixing  is  slow  and  regular.  After  mixing  the  product  is  washed 
with  water  to  remove  the  surplus  acid.  The  solid  nitroglycerine  is 
made  into  cylindrical  forms  and  has  the  appearance  of  a  yellowish 
transparent  jelly.  It  has  the  consistency  of  rubber  and  can  be  readily 
handled  without  danger,  both  during  transportation  and  at  the  well. 

The  process  and  product  are  patented.  The  liquid  explosive  is  pre- 
ferred because  of  its  efficiency.  The  standard  prices  for  the  explosive 
are  as  follows : 

Quarts.  Value. 

10    $25  00 

20 40  00 

30     47  50 

40     55  00 

60  and  more,  per  quart 1  15 

Other  charges  include  2  cents  per  foot  for  electric  wiring,  and  in 
case  of  delay,  an  extra  charge  of  $15.00  per  day  for  the  time  of  the 
shooter. 

Lease  Equipment. 

cleaning  out  and  tubing  the  well. 

After  the  well  has  been  shot  and  a  production  of  oil  assured,  the 
drillers  clean  it  out  in  a  manner  similar  to  the  original  drilling.  The 
bit  is  worked  through  any  accumulated  debris  and  the  bailer  brings  up 
the  slush.  The  pocket  or  cavity  is  emptied  and  thus  serves  as  a  reser- 
voir. A  two-inch  tubing,  containing  a  5/8  inch  sucker  rod  and  cup, 
usually  placed  in  the  casing  to  the  sand  and  is  connected  to  the  pumping 
machinery.  If  the  well  is  the  first  one,  the  rod  is  set  to  pumping 
directly  from  the  walking  beam.  If  the  well  is  one  of  several,  it  is 
connected  to  the  power-house  by  a  pumping  jack.  A  three-inch  tubing 
is  often  used  if  the  well  is  a  large  one  or  large  quantities  of  salt  water 
are  encountered.  The  cost  of  tubing  is  liy2  cents  per  foot.  During 
the  life  of  the  well  cups  often  become  worn  or  loose  and  are  repaired 
by  the  use  of  a  portable  cleaning  rig.      (See  PI.  XXVII,  B.) 

TANKS. 

The  oil  from  the  first  well  is  sent  to  emergency  tanks  and  from  later 
wells  to  the  lease  tanks.  The  tanks  are  usually  low  cylinders,  built  of 
wooden  staves  and  steel  bands.  They  range  from  100  to  1,600  barrels 
capacity.  The  smaller  tanks  are  transported  to  a  well  when  oil  is 
found  and  are  used  to  receive  the  supply  until  the  permanent  lease  tanks 
are  located  and  built.  The  usual  250-barrel  tank  measures  2%  barrels 
of  oil  to  the  inch  or  25  barrels  to  ten  inches  of  depth.     The  cost  of  this 


158  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

size  tank  is  about  $90,  and  of  the  1,600-barrel  tank  about  $450.  Second- 
hand 250-barrel  tanks  cost  about  $50  and  are  preferred  because  they 
are  saturated  with  oil  and  less  liable  to  leakage.  When  several  tanks 
have  been  built  on  a  lease,  sheds  are  placed  over  them  for  protection 
from  evaporation  and  to  prevent  their  warping  by  the  sun's  heat.  (See 
PL  XIX,  A.)  The  average  cost  of  these  is  about  $60,  although  the 
cost  is  dependent  upon  the  size. 


LOADING    RACKS. 

The  oil  from  a  new  field  is  generally  sent  by  donkey-pump  to  the 
nearest  railway  loading-rack  (see  PL  XX,  B)  and  is  shipped  by  tank- 
car  to  the  refineries  or  to  manufacturing  companies  who  have  use  for 
crude  oil.  The  racks  are  usually  composed  of  upright  tubing  of  about 
two  or  three  inches  in  diameter  with  swinging  ends  that  fit  into  the 
mouths  of  the  tank  cars.  They  are  connected  direct  to  the  pipe  lines 
from  the  lease.  The  loading  racks  that  are  maintained  in  the  fields  at 
present  are  provided  with  facilities  for  measuring  the  exact  amounts  of 
oil  shipped  (see  PL  XX,  A).  Loading  racks  are  installed  at  Bridge- 
port and  Lawrenceville  on  the  Baltimore  and  Ohio  railroad;  Lawrence- 
ville,  Birds,  Flat  Rock,  and  Robinson,  on  the  Big  Four  railroad;  Robin- 
son, Stoy,  Bakers  Lane,  and  Oblong  on  the  Illinois  Central  railroad; 
Casey  and  Oilfield  on  the  Cincinnati,  Hamilton  and  Dayton  railroad; 
and  Casey  and  Martinsville  on  the  Vandalia  railroad. 


POWER   AND   BOILER    HOUSES. 

With  four  or  five  wells  on  a  lease  it  becomes  practicable  to  build  a 
centrally  located  power-house  for  pumping  them.  The  walls  of  the 
building  are  constructed  of  wood  or  corrugated  sheet-iron,  and  the 
floors  of  cement  (see  PL  XXI,  A).  A  gas  engine  is  installed  at  one 
end  of  the  building,  and  at  the  other  end  an  oscillating  pull-wheel  to 
give  horizontal  movement  to  the  surface  rods  radiating  from  it  to  the 
different  wells.  The  pull-wheel  draws  the  surface  rod  toward  the  power 
and  the  weight  of  the  sucker  rod  in  the  well  assists  in  pulling  it  back, 
thus  providing  the  necessary  balance  of  work,  A  boiler-house  is  built 
close  to  the  power  house  for  emergency  use  and  for  steaming  the  oil 
(see  PL  XXI,  B).  The  average  cost  of  the  power-house  and  boiler- 
house  is  about  $1,200.  The  25-H.  P.  gas  engines  cost  $425;  the  35- 
H.  P.  engines,  $585;  the  Mascot  power,  $320,  and  the  boiler,  $385. 
One  equipment  serves  as  many  as  40  wells,  but  usually  only  25  to  30. 
The  power  man  in  charge  can  not  look  after  more  than  this  number  and 
accomplish  his  daily  work.  The  power  man  makes  the  rounds  of 
inspection,  cares  for  his  engine,  boiler  and  oil  tanks,  and  makes  a  daily 
report.  It  often  becomes  necessary  on  the  larger  leases  to  employ  a 
helper.  He  is  called  the  "roust-a-bout"  and  assists  the  power  man 
in  looking  after  the  wells.  The  power  fuel  is  usually  gas  and  is  gen- 
erally piped  from  the  wells  in  the  lease.  Some  leases  do  not  produce 
gas  and  it  is  then  bought  from  another  lease  or  from  a  nearby  gas 
line.     Steam  is  used  if  the  lease  is  isolated  or  gas  cannot  be  secured. 


ILLINOIS    STATE    GEOLOGICAL   SURVEY. 


Bull.   No.    22,   Plate  XXII. 


A.  The    standard    pumping-jack. 

B.  The   steel   pumping- jack. 


blatchley]  EQUIPMENT  OF  OIL  LEASES.  159 

PULL-RODS    AND    PUMPING    DISCS. 

The  surface  pull-rods  are  generally  made  of  steel  or  wire  cable.  They 
are  supported  in  a  level  line  to  the  well  by  posts  of  various  lengths,  de- 
pending upon  the  undulations  of  the  farm.  Notches  are  cut  in  the  top 
of  the  posts  for  guiding  the  lines,  and  are  greased  occasionally  to 
minimize  the  friction  of  the  rod.  Wells  may  be  pumped  in  spite  of 
intervening  buildings  or  two  wells  may  be  attached  to  one  general  lead- 
line by  the  use  of  suitable  angle-knees.  Large  flat,  oscillating  pumping 
discs  are  often  used  to  overcome  surface  irregularities  or  obstructions, 
and  for  pumping  across  highways  (see  PL  XIX,  B).  They  are  placed 
in  the  open  field  and  are  connected  to  the  power  by  large  pull-rods, 
which  move  alternately  and  turn  the  disc  through  an  arc  of  about  one- 
fifth  of  a  circle.     Surface  rods  radiate  from  the  disc  to  the  wells. 

PUMPING  JACKS. 

The  standard  wooden  jack,  steel  jack  and  "home-made"  wooden  jacks 
are  used  in  Illinois.  The  standard  jack  is  substantially  mounted  over 
the  well  on  heavy  wooden  sills.  (See  PL  XXII,  A.)  The  workable 
portions  resemble  a  right  triangle,  with  the  right  angle  pivoted,  the 
upper  acute  angle  fastened  to  the  sucker  rod,  and  the  lower  acute  angle 
to  the  surface  rod.  The  pull-wheel  draws  the  lower  angle  outward  and 
at  the  same  time  raises  the  upper  angle  and  sucker  rod.  When  the 
stroke  is  made  the  weight  of  the  sucker  rod  pulls  the  jack  to  its  normal 
position.  The  steel  jack  is  similar  to  the  standard  wooden  jack  except 
for  materials  and  weight.  (See  PL  XXII,  B.)  With  the  home-made 
jack  the  angles  are  reversed  and  the  action  is  one  of  pushing.  (See 
PL  XXIII,  A.)  Light  weight  jacks  cost  about  $10.00  and  heavy  ones 
about  $17.00.  Sometimes  wells  are  so  arranged  that  the  working 
balance  between  sucker  and  surface  rods  is  uneven.  In  this  case  ad- 
justment is  made  by  weights  upon  the  jack  to  push  the  sucker  rod  down 
or  by  weights  at  other  points  to  aid  the  pull-rod. 

REMOVAL  OP  SALT  WATER  AND  STEAMING  OIL. 

Salt  water  often  accompanies  the  oil  into  the  tanks  and  by  difference 
in  weight  finds  its  way  to  the  bottom  where  it  is  withdrawn  by  opening 
a  bung-hole.  It  is  the  usual  practice  to  run  the  oil  into  separating 
tanks  where  a  siphon  is  so  set  that  the  oil  runs  one  way  into  the  lease 
tanks  and  the  water  flows  in  another  direction  into  nearby  streams. 
The  oil  often  roils  and  assumes  a  yellowish  color  when  it  is  pumped  too 
hard.  This  is  due  to  a  suspension  of  sulphur  which  interferes  with  re- 
fining. The  removal  of  the  sulphur  and  other  impurities  is  accomplished 
by  precipitation  with  steam,  usually  for  three  hours  in  a  250-barrel 
tank.  The  sediment  is  piped  away  from  the  bottom  of  the  tank  to  a 
shallow  pit  some  distance  from  the  buildings,  where  it  is  burned  and 
prevented  from  polluting •  the  streams.  (See  PL  XXIV,  A.)  The 
waste  pit  is  a  shallow  hole  in  the  ground  surrounded  by  a  small  dike. 
It  is  usually  constructed  at  a  lower  elevation  than  the  tanks  in  order  to 
provide  a  flow  by  gravity.  A  recent  investigation  by  federal  officials 
has  put  a  stop  to  running  waste  oil  into  streams.     It  is  claimed  that 


160 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22" 


the  waste  has  killed  many  fish  and  contaminated  the  water  in  the  Em- 
barrass and  Wabash  rivers.  During  freshets,  it  has  saturated  the 
foliage  and  underbrush  along  their  tributaries,  and  in  several  cases,, 
this  was  later  destroyed  by  fire.  (See  PL  XXIV,  B.)  The  pollution 
of  the  streams  is  not  only  unsightly  but  the  waste  becomes  offensive  after 
having  stood  through  the  heat  of  a  summer.  It  is  true,  however,  that 
the  streams  cannot  be  freed  entirely  from  waste  because  the  surplus 
salt  water  must  be  taken  care  of.  The  present  system  of  burning  has 
greatly  minimized  the  problem. 


The  Approximate  Cost  of  Oil  Wells. 

The  following  table  presents  the  approximate  cost  of  the  first  wells 
and  the  lease  equipment  in  the  various  Illinois  pools: 


Cost  of  Wells  and  Their  Equipment  in  Illinois. 


o 
o 

M 

5 

B 
o 
o 

o 
Q 

Lawrence  county. 

Items. 

o 

&  . 

©irj 

29 

G 
PI     • 

pq 

t3 
o 
o    . 

■5    02 

Eh 

49 

u 

Rig 

$    500 
700 

90 
800 

90 
150 
1,200 
250 
100 
100 

$    500 
750 

90 
900 

90 
150 
1,200 
250 
100 
100 

$    500 

1,750 

90 

1,700 

100 

200 

1,200 

250 

100 

100 

$    500 

2,300 

90 

2,800 

100 

215 

1,200 

250 

100 

100 

$    500 

2,500 

90 

3,400 

100 

250 

1,200 

250 

100 

100 

$    500 

Drilling 

3    360 

80 

250 

90 

150 

1,200 

250 

100 

100 

2,800 
90 

Drive-pipe 

Casing 

3  80O 

Shooting 

'  100 

Tubing  and  pumping  outfit 

250 

Power  and  boiler-house  equipment 

Tanks  and  sheds 

1,  200 
250 

Belting  and  lead  lines 

100 

Incidentals ...     . 

100 

Total 

$2,580 

$3,980 

$4, 130 

$5, 990 

$7,655 

$8, 490 

$9, 19a 

The  above  figures  may  be  increased  considerably  if  trouble  is  en- 
countered in  drilling  the  well  or  if  the  well  is  situated  at  a  considerable 
distance  from  transportation.  The  second  and  succeeding  wells  cost 
less  than  the  first  one  by  about  $1,700.00  in  Clark  county,  $2,400.00  in 
Crawford  county,  $2,300.00  for  those  in  the  Bridgeport  sand,  $2,800.00 
for  those  in  the  Buchanan  sand,  $2,900.00  for  those  in  the  Kirkwood 
sand,  $3,500.00  for  those  in  the  Tracey  sand,  and  $3,800.00  for  those 
in  the  McClosky  sand.  The  rig,  drive-pipe,  a  portion  of  the  casing, 
tanks  and  power  and  boiler-house  equipment  serve  for  several  wells. 
The  incidentals  include  the  expenses  of  the  operator  and  the  cost  of 
teaming,  which  is  dependent  upon  available  teamsters  and  the  amount 
of  work  being  done,  but  which  averages  $4.50  per  day.  The  weights  of 
the  various  sizes  of  casing  most  commonly  used  are, 

10-inch     • 32  lbs.  per  foot 

814-inch     24  lbs.  per  foot 

6  5/8-inch    13  lbs.  per  foot 

The   general   cost   of   drive-pipe,   casing,   tubing   and   rodding   is   as 
follows : 


ILLINOIS    STATE    GEOLOGICAL    SURVEY. 


Bull.    No.    22,    Plate   XXIIJ. 


B. 


A.  A   third    type    of   pumping- jack. 

B.  A  town-lot  well  in   Bridgeport,   111. 


BLATCHLEY] 


COST   OF   OPERATING  A   LEASE. 

Cost  of  Well  Supplies  in  Illinois. 


161 


Diameter — 
inches. 


Cost  per 
foot. 


Drive-pipe 

Casing  (No.  50). 
Casing  (St'd)... 

Casing 

Casing 

Casing 

Casing 

Tubing 

Oil  line 

Gas  line 

Sucker-rods 

Pull-rods 


S3. 25 
2.15 
1.24 
1.09 
0.728 
0.5195 
0.407 
0.12 
0.098 
0.885 

*4.04 

*3.57 


*  Per  hundred  feet. 


An  idea  of  the  enormous  amount  of  casing  and  supplies  used  in  the 
Lawrence  county  district  is  presented  in  Plate  XXX. 


The  Cost  of  Operating  a  Lease. 

The  cost  of  operating  a  lease  does  not  vary  noticeably  in  the  several 
Illinois  pools  and  indeed  is  often  negligible  when  compared  with  the 
earning  power  of  the  wells.  The  high  cost  of  development,  the  interest 
on  the  investment,  and  the  expense  of  plugging  wells  are  the  barriers 
to  be  overcome,  particularly  in  the  deep  sand  areas  of  Lawrence  county 
before  profits  accrue  to  the  operators.  The  shallow  fields  of  Clark 
county  have  been  among  the  most  profitable  in  the  world  because  of  the 
low  cost  of  development  and  the  high  returns.  On  the  other  hand  the 
deep  wells  of  Lawrence  county  have  been  just  as  profitable  perhaps,  but 
the  expense  of  development  has  been  very  high.  This  was  overcome  by 
a  high  and  steady  production.  The  Crawford  county  area  has  been  a 
valuable  and  safe  field  because  of  the  steady  yield  of  the  wells  and  a 
rather  low  cost  of  development.  The  first  wells  in  any  field  usually 
hold  up  better  than  later  wells  and  naturally  produce  more  oil,  prob- 
ably because  the  openings  were  made  permanent  under  stress  or  pres- 
sure, etc.  The  essential  feature  in  operating  is  to  overcome  first  cost 
and  the  interest  on  the  investment.  In  the  shallow  fields  eight  wells* 
steadily  making  two  and  even  one  barrel  per  day  are  found  to  be  profit- 
able. One  company  has  operated  100  old  wells  for  two  years  that  yielded 
totally,  150  to  300  barrels  per  day.  The  total  cost  of  operation  was 
$600.00  per  month.  The  yield  of  oil  gave  an  average  net  income  of 
$3,000.00  per  month,  with/ a  maximum  of  $7,000.00  per  month.  The 
minimum  cost  of  operating  a  lease  should  average  about  $120.00  per 
month  while  the  maximum  should  be  about  $160.00.  The  pumper 
receives  $66.00  for  care  of  a  light  lease  and  about  $72.00  for  two 
small  leases  or  a  large  one.  The  sum  of  $20.00  is  required  for  fuel, 
although  the  gas  cost  is  usually  low  or  nothing,  and  $30.00  for  teaming 
and  supplies. 

In  a  declining  field,  after  the  cost  of  development  has  been  met,  it 
has  been  found  profitable  to  pump  three  or  four  wells  of  5-barrel  capa- 

—11  G 


162  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

city.  The  monthly  output  from  four  5-barrel  wells,  after  deducting  a 
royalty  of  one-sixth,  is  500  barrels.  At  the  current  price  of  67  cents 
per  barrel  January  1,  1912,  the  income  is  as  follows: 

Five  hundred  barrels  at  67  cents $335  00 

Cost  of  operating 140  00 

Net  income    ,  $170  00 

The  net  income  from  ten  5-barrel  wells  or  five  10-barrel  wells  would 
be  about  $700.00  per  month. 

INVESTMENTS  IN  OIL  PROPERTIES. 

Investments  in  oil  properties  fall  naturally  into  two  classes — those  in 
the  wild-cat,  or  unproven  territory,  and  those  in  developed  fields.  One 
deals  with  chance  and  the  other  is  largely  a  definite  business  venture. 

An  investment  in  a  wild-cat  scheme  is  at  all  times  uncertain  because 
there  is  no  assurance  of  finding  oil.  Wild-cat  work  is  necessary  for  the 
development  of  any  oil  territory,  but  it  should  be  left,  if  possible,  to 
those  large  companies  which  have  a  reserve  fund  for  such  purpose. 
These  companies  are  in  a  position  to  drill  several  wellp  before  oil  is  found 
or  the  venture  abandoned.  The  basis  of  wild-cat  work  may  be  a  geolog- 
ical study,  surface  seepage  or  a  previous  exploitation  of  some  kind.  The 
area  in  consideration  is  then  leased,  often  in  lots  as  much  as  40,000 
acres,  which  in  case  oil  is  found,  would  naturally  protect  the  interests 
of  the  active  operators.  The  only  definite  knowledge  the  prospecting 
company  might  have  in  unproven  territory  would  be  the  result  of  the 
work  of  a  competent  geologist.  This  knowledge  should  lead  the  com- 
pany from  drilling  in  the  basins,  which  would  probably  be  full  of  salt 
water  and  afford  little  promise  of  the  presence  of  oil,  to  raised  struct- 
ures where  conditions  for  the  accumulation  of  oil  are  more  favorable. 
The  drilling  bit  alone  will  give  evidence  of  the  actual  presence  of  oil 
or  its  absence.  The  man  of  small  means  should,  for  his  own  protec- 
tion, beware  of  venturing  into  new  territory  but  should,  if  possible, 
join  a  responsible  oil  company  that  intends  to  purchase  a  proven  prop- 
erty and  develop  it  as  such.  He  could  lease  and  drill  only  in  a  limited 
area  and  one  or  two  unsuccessful  attempts  would  force  him  to  abandon- 
ment. It  has  happened,  however,  that  in  some  instances  the  small 
operator  has  been  successful  and  has  opened  up  a  field,  but  experience 
proves  that,  generally,  the  case  is  otherwise. 

Investments  in  developed  fields  are  matters  of  calculation  and  judg- 
ment. A  usual  custom  of  a  purchasing  company  is  to  send  representa- 
tives into  a  field  to  carry  on  a  ten-day  gauge  on  those  properties  the 
buying  of  which  is  under  consideration.  At  the  end  of  this  time  the 
value  of  the  property  is  rated  at  a  definite  amount  per  barrel  of  the 
average  daily  yield  of  the  lease.  The  usual  price  per  barrel  for  future 
production  is  about  $400,  though  it  often  reaches  $500  or  more,  if  a 
property  is  particularly  desirable.  If  a  40-acre  lease  produces  steadily 
500  barrels  of  oil  per  day,  the  buying  price  would  be  500x400  or 
$200,000.00.  Under  this  investment  a  property  with  a  reasonable  decline 
should  pay  for  itself  in  about  three  years.     There  is  some  opportunity 


ILLINOIS    STATE   GEOLOGICAL    SURVEY. 


Bull.   No.    22,   Plate   XXIV. 


11'  WMfcf  l , 

i 

Mk-wmmihl  i  i 

WwIWnI  II  Itj 

itfmrmfYirii  III   i '  111'  M^yii 

■ 

\  rm  w  B! 

Pi 

ttffci 

"ff  w)  l-irtii 

■  1 
I  i 

B. 


A.  A   waste   pit   for   burning   waste    oil. 

B.  The   effect   of  fire   from   waste   oil   on   streams. 


blatchley]  INVESTMENTS   IN   OIL.  163 

of  failure  even  in  producing  areas  through  a  sudden  drain  of  the  sands 
or  a  flooding  of  the  area  with  salt  water. 

The  actual  amounts  of  oil  won  per  acre  are  variable.  Some  portions 
of  the  field  have  yielded  6,000  barrels  per  acre  and  are  still  producing, 
though  not  extensively.  Other  portions  with  wells  equally  good  in 
initial  production  have  yielded  Only  500  barrels  or  less  per  acre.  One 
tract  produced  10,000  barrels  per  acre  and  from  another  of  20  acres 
over  a  million  barrels  of  oil  were  taken.  The  last  was  only  possible 
because  the  owner  built  his  own  storage  tanks  and  pumped  constantly. 
It  is  evident  that  this  shrewd  gentleman  secured  some  oil  which  would 
have  gone  to  his  neighbors  had  they  been  similarly  provided  with 
storage. 

The  deeper  and  more  prolific  sands  of  Lawrence  county  have  yielded 
much  greater  quantities  of  oil  and  perhaps  will  continue  to  do  so,  be- 
cause of  the  several  producing  sands  and  the  remarkable  staying  quali- 
ties of  the  wells.  This  area  will  probably  be  productive  for  a  good  many 
years,  as  has  been  the  case  in  the  Appalachian  region.  The  shallower 
fields  to  the  north  with  one  sand,  or  two  or  more  lenses  of  the  same 
sand,  are  already  showing  signs  of  decline.  The  combined  daily  output 
of  the  Clark,  Cumberland  and  Edgar  county  wells  on  January  "l,  1912, 
was  about  9,000  barrels  as  against  about  40,000  barrels  in  1907.  The 
Crawford  county  yield  reached  about  20,000  barrels  daily,  as  against 
100,000  barrels  in  1907.  The  Lawrence  county  production  has  steadily 
increased  since  the  first  development  and  at  the  present  time  produces 
more  than  the  rest  of  the  counties  combined  and  about  double  that  of 
Crawford  county. 

Since  the  Illinois  fields  were  discovered,  many  men  wishing  to  invest 
have  found  that  the  field  was  completely  leased  and  that  the  only  oppor- 
tunity to  share  in  the  business  was  to  join  an  established  company  or 
to  organize  a  new  company  to  buy  partially  or  wholly  developed  tracts. 
Even  this  has  been  difficult  because  of  the  enormous  prices  asked  for 
good  leases  and  the  scarcity  of  stocks  of  organized  and  prosperous  com- 
panies. 

The  transfer  of  oil  properties  has  been  common  in  the  last  two  years 
and  has  comprised  dealings  in  both  developed  and  undeveloped  leases. 
The  Ohio  Oil  Company,  the  producing  agent  of  the  Standard  Oil  Com- 
pany, has  been  the  most  active  purchaser  of  producing  properties  in 
Illinois.  It  has  recently  bought  out  many  large  companies  such  as  the 
Jennings  Oil  Company,  Parker  and  Edwards,  Kiddle  Oil  Company, 
Brown  and  Hogue,  The  Lee  Oil  Company,  The  North  Fork  Oil  Com- 
pany, and  other  smaller  companies.  Before  these  purchases  it  owned 
and  operated  leases  to  the  amount  of  about  40  per  cent  of  the  fields. 
Its  total  holdings  now  are  probably  more  than  70  per  cent  of  the  total 
development.  This  company  buys  and  stores  more  than  90  per  cent  of 
the  oil  of  the  State.  How  much  of  the  production  comes  from  its  own 
Leases  is  not  known,  but  certainly  not  less  than  half. 

BUYING,  TRANSPORTING  AND  STORING  OIL. 
Buying  Oil. 
When  the  oil  is  steamed  and  ready  to  be  sold,  the  power  man  notifies 
;he  gauger  of  the  Ohio  Oil  Company  or  the  Indian  Refining  Company, 


164 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


who  determines  the  quality  and  quantity  of  oil  on  each  lease.  A  report 
or  "ticket"  is  made  and  signed  by  the  gauger  and  lease  man  and  copies 
are  retained  by  each  while  an  additional  one  is  sent  to  the  purchasing 
company's  office.  The  purchasing  company  enters  the  report  on  its 
books  and  in  a  short  time  checks  are  made  out  individually  to  all  parties 
interested  in  the  transaction  under  what  are  termed  division  orders.  A 
division  order  is  a  tabulated  form  including  signed  and  sworn  state- 
ments that  the  operator  has  a  certain  interest  in  a  producing  company 
or  in  a  lease  and  that  the  landowner  has  a  royalty,  usually  one-eighth 
of  the  oil.  The  division  order  is  kept  on  file  with  the  purchasing  com- 
pany. A  producer  can  hold  his  oil  in  storage  for  two  months,  and  at 
the  expiration  of  that  time  checks  are  sent  at  the  prevailing  price.  The 
purchasing  company  pro-rates  its  own  leases  as  it  does  those  of  in- 
dividual operators  and  issues  royalty  checks  directly  to  the  farmer.  In 
all  reports  3  per  cent  of  the  gauged  oil  is  deducted  for  leakage,  sediment 
and  evaporation,  which  goes  on  continually  until  the  oil  reaches  the 
refinery.  This  is  a  natural  loss  and  is  borne  by  all  interested  in  the 
production. 

The  auditing  department  of  the  Ohio  Oil  Company,  Marshall,  111.,  has 
one  of  the  most  complete  systems  of  its  kind.  The  amount  of  work 
done  by  it  is  enormous,  and  its  thoroughness  is  attested  by  the  scarcity 
of  complaints  from  either  landowner   or  operator. 

Transporting  the  Oil. 
The  Ohio  Oil  Company  is  not  a  common  carrier  of  oil,  but  is  a 
buyer.  The  old  system  of  carrying  oil  at  a  certain  rate  in  addition  to 
storage  has  disappeared.  During  1907  and  1908  the  Ohio  Oil  Company 
built  an  extensive  system  of  gravity  pipe-lines  for  collecting  oil  from 
the  greater  part  of  the  field.  E.  C.  Bolton,  chief  engineer,  made  thorough 
detailed  surveys  of  all  the  leases  and  all  the  stream  courses  through  or 
near  the  field.  Advantage  was  taken  of  the  slope  of  the  streams  and 
pipe-lines  were  laid  along  them.  Branch  lines  were  run  to  each  lease 
so  that  the  oil,  when  released  from  the  lease  tanks,  flows  by  its  own 
weight  into  the  general  stream  main,  and  down  its  course  to  a  sub- 
station, where  it  is  caught  and  pumped  back  through  a  larger  main  to 
the  head  pumping  station  at  Martinsville,  111.  There  are  thirteen  sub- 
stations in  the  main  fields  and  one  at  Sandoval,. 111.,  located  as  follows: 


Location  of  the  Ohio  Oil  Company's  Pumping  Stations  in  Illinois.1 

Order 

Station— name. 

Section. 

Township. 

County. 

1 

7 

2 

9 

17 

23 

20 

1 

13 

29 

14 

13 

6 

11 

7 

Martinsville 

Oblong 

Lawrence 

Clark 

2 

Stoy 

Crawford  (see  PI.  XXV  A). .. 

3 

Lawrence  (see  PI.  XXVI).. . . 

4 

Casey 

Clark 

5 

Union 

Cumberland 

6 

Petty 

Lawrence 

7 

North  Fork 

Licking 

Crawford 

g 

Clark 

9 

Martin 

Crawford 

10 

Oblong 

..do 

11 

Lawrence 

Lawrence. 

12 

Dennison 

..do 

13 

Martin 

Sandoval 

Crawford 

14 

Sandoval    .           

Marion 

i  Kindly  furnished  by  D.  Roach,  chief  of  pipe-line  department,  Ohio  Oil  Co.,  Marshall,  111. 


ILLINOIS    STATE    GEOLOGICAL   SURVEY. 


Bull.  No.    22,   Plate   XXV. 


X 

■ 

;*J ''                                       ^ 

1                                                                        * 

foB    B  1 

fcl-?"g 

^^g 

^M                                      II                                   V 

m  -•-^^i 

k                          vf 

HBriBnt 

i  f] 

,.  -    -  -~_««a«KS»  user.  «*•«*«" 

li;B 

i 

^saR^^i^ 

: 

B. 

A.  The  Ohio  Oil   Company's  pumping  station,   Stoy,   111. 

B.  The   Tidewater   Pipe    Line    Company's    pumping-   station,    Stoy,    111. 


blatchley]  HANDLING  OF  OIL.  165 

Each  station  controls  the  area  north  of  it  to  the  next  station.  From 
the  head  station  at  Martinsville,  the  oil  is  pumped  through  one  12-inch 
and  two  8-inch  pipes  across  Indiana  and  Ohio  to  eastern  refineries,  and 
through  one  8-inch  to  Alton,  111.  The  inter-state  pipe-lines  are  pumped 
in  relays,  with  sub-stations  at  Jamestown  and  Montpelier,  Ind.,  and  at 
Lima,  Ohio.     Oil  is  pumped  at  about  600  pounds  pressure  in  the  lines. 

Gravity  has  displaced  the  old  donkey  pump  that  was  formerly  required 
on  each  lease,  except  in  the  extreme  northern  end  of  the  field.  The 
gravity  lines  extend  northward  within  2%  miles  south  of  Casey.  The 
donkey  pump  is  still  used  in  this  area.  The  Ohio  Oil  Company  pays 
one  cent  per  barrel  to  the  producers  for  steam  used.  The  efficiency  of 
the  gravity  system  is  twice  as  great  as  with  steam  and  the  cost  is  one- 
third  as  great.  The  cost  of  transfer  by  the  gravity  system  is  borne  by 
the  Ohio  Oil  Company.  A  regular  force  of  men,  aside  from  the  com- 
pany^ corps  of  surveyors  is  kept  at  work  improving  and  repairing  the 
lines.  The  company  keeps  apace  with  new  development  and  supplys 
new  lines  at  fast  as  they  are  needed. 

The  Ohio  Oil  Company  maintains  engineering  and  surveying,  dis- 
charge, and  telegraph  departments  in  its  general  offices  at  Marshall,  111. 
The  engineering  and  surveying  department  surveys  and  outlines  sites 
for  pipe-lines,  pumping  stations,  tank  farms,  power-houses,  district 
supply-houses,  etc.  It  makes  all  field,  farm,  tank-farm,  road  and  pipe- 
line maps.  In  fact,  this  branch  of  the  work  covers  completely  all  the 
phases  of  work  connected  with  civil  engineering.  It  is  occasionally 
called  upon  to  make  plans  of  specially  needed  machinery,  or  the  con- 
struction of  some  special  type  of  building.  As  yet  these  departments 
have  done  little  toward  determining  structural  relations  of  the  forma- 
tions and  working  out  geological  problems  dependent  upon  this  phase  of 
work. 

The  discharge  department  has  charge  of  the  pumping  of  oil.  This 
division  merely  regulates  and  checks  the  pumping  of  the  oil  into  and 
through  the  interstate  lines.  The  telegraph  department  of  the  company 
consists  of  a  complete  system  of  telegraph  lines  to  all  portions  of  the 
field,  thus  bringing  its  large  force  of  employees  into  close  touch  with 
headquarters.    Wires  are  also  maintained  and  operated  to  eastern  offices. 

Storing  the  Oil, 

The  production  of  the  Illinois  fields  so  far  exceeds  the  capacity  of 
pipe-lines  that  storage  tanks  have  been  established.  Permanent  tank 
farms  are  maintained  at  Martinsville,  Stoy  and  Bridgeport.  (See  PI. 
XXVII,  A.)  The  sub-stations  discharge  the  surplus  oil  to  these  tanks, 
where  it  lies  until  it  can  be  pumped  to  the  refineries.  The  Ohio  Oil 
Company  has  471  storage  tanks  which  hold  about  35,000  barrels  each. 
These  tanks  are  distributed  in  the  oil  producing  counties  of  Illinois  as 
follows : 

Clark .' 235 

Crawford    43 

Lawrence 192 

Marion 1 

Total 471 


166  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

The  cost  of  each  tank,  including  a  circular  dike  for  catching  the  oil 
in  case  the  tank  bursts  or  catches  fire,  is  about  $9,000.00.  The  tanks 
are  made  of  riveted  steel  plate,  measuring  y2  inch  thick  at  the  bottom 
and  on  the  floor,  and  3-16  inch  thick  at  the  top.  They  are  95  feet  in 
diameter  and  28  feet  7y2  inches  high.  The  floor  space  is  7,200  square 
feet.  The  total  investment  in  tank-farms  and  equipment  is  about 
$5,000,000.00.  Other  large  companies  maintain  tanks,  but  they  are 
scattered  singly  over  the  field. 

Lightning  has  occasional  heavy  losses  on  tank  farms.  At  least  one 
dozen  tanks  have  been  destroyed  in  the  last  two  years.  (See  PL 
XXVIII.)  Lightning  pierces  the  tanks  easily  and  sets  fire  to  the  gases 
and  oils.  In  a  short  time  the  top  of  the  tank  drops  in  and  the  flames 
send  up  dense,  black,  curling  smoke,  which  presents  a  most  unusual  and 
startling  spectacle.  It  requires  about  24  hours  for  the  entire  contents 
of  a  tank  to  boil  over  its  sides  and  50  hours  for  the  fire  to  burn  out. 
At  the  time  of  boiling  the  smoke  and  danger  are  greatest.  If  the  wind 
should  be  blowing  strongly,  any  buildings,  timber,  or  nearby  tanks  would 
probably  be  destroyed.  The  Ohio  Oil  Company  always  rushes  a  large 
force  of  men  to  the  scene  of  a  fire  and  takes  every  precaution  to 
minimize  the  loss  by  strengthening  the  dike  and  removing  inflammable 
material.  The  nearest  pumping  station  is  called  upon  to  connect  with 
the  burning  tank  and  draw  out  as  much  oil  as  possible  with  safety, 
usually  about  half  the  amount  in  the  tank.  The  loss  by  fire  of  a  tank 
full  of  oil  is  about  $20,000.00.  The  heat  thrown  off  from  a  tank  fire  is 
intense  and  the  effect  on  the  tank  is  disastrous.     (See  PI.  XXIX.) 


Independent  Oil  Companies. 

The  independent  operators  and  oil  companies  have  been  forced  to 
rely  on  tank-cars  for  oil  shipments  until  recently,  or  to  sell  to  the  Ohio 
Oil  Company.  Most  of  them  have  preferred  the  latter  plan.  The  Tide- 
water Pipe  Line  Company,  with  the  Associated  Producers  Oil  Company, 
however,  has  recently  built  an  8-inch  line  into  the  field  and  constructed 
a  pumping  station  near  Stoy,  Crawford  county,  with  a  capacity  of  about 
25,000  barrels  daily.     (See  PL  XXV,  B.) 

The  Pure  Oil  Company  which  has  been  a  large  producer  in  this  field, 
is  said  to  have  bought  right  of  way  for  a  second  independent  pipe-line. 
The  Indian  Eefining  Company  of  Cincinnati  and  New  York  has  over 
500  tank  cars  and  30  distributing  stations,  with  refineries  at  George- 
town, Ky.,  Lawrenceville,  and  East  St.  Louis,  111.;  a  combined  capacity 
of  about  8,000  barrels  per  day.  The  Sun  Oil  Company  ships  by  tank 
cars  and  sells  its  oil  for  fuel.  The  Missouri-Illinois  Oil  Co.  operates 
in  St.  Louis,  Mo.  The  Central  Refining  Company  has  a  refinery  at 
Lawrenceville  and  secures  oil  from  its  own  leases.  The  other  com- 
panies that  make  shipments  from  the  fields  are  the  Cornplanter  Refining 
Company,  W.  F.  Watson  of  Bridgeport,  111.,  and  Rogers  and  Dibble  of 
Oil  City,  Pa.  It  is  estimated  that  the  independents  are  handling  be- 
tween 9,000  and  12,000  barrels  of  oil  per  day.  The  Robinson  Oil  Re- 
fining Co.  maintained  a  small  plant  at  Robinson  until  the  latter  part  of 
1908,  when  it  fell  into  the  hands  of  a  receiver  and  has  since  been  idle. 


BLATCHLEY]  PRICES    OF    ILLINOIS     OIL.  167 

PRICES  AND  PIPE-LINE  RUNS  OF  ILLINOIS  OIL. 

Prices  of  Illinois  Oil, 

The  price  of  Illinois  oil  increased  steadily  from  the  opening  of  the 
field  in  1905  to  July  of  1906.  From  1907  to  November,  1909,  the 
decline  was  gradual.  The  price  then  remained  steady  for  18  months 
and  since  May,  1911,  has  begun  to  increase.  From  1905  to  1907  in- 
clusive all  oil  sold  at  one  price,  varying  from  60  to  83  cents  per  barrel. 
A  grading  and  division  in  price  took  place  in  1908.  The  better  grades 
of  oil  were  found  to  lie  between  30  and  35°  B,  while  that  of  the  Dun- 
canville  pool  lies  between  22  and  23°  B.  The  Duncanville  oil  is  sold 
only  for  fuel.  The  development  of  the  Tracey  and  McClosky  sands  in 
Lawrence  county  gave  still  higher  grades  of  oil,  varying  from  35  to 
39°  B.  The  difference  of  gravities  necessarily  caused  a  division  of  price 
and  since  1908,  oil  above  30°  B  has  commanded  one  price  while  that 
below  30°  B  has  commanded  another.  The  following  table  gives  the 
average  monthly  prices  paid  for  Illinois  petroleum  from  1905  to  191% 
inclusive,  as  reported  by  Dr.  D.  T.  Day  and  to  January  1,  1912,  thi 
date  of  completion  of  this  report,  as  supplied  by  the  writer: 


168 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


2§5 


1« 


■<  CO 


<J  CO 


■<  CO 


U5  K5  «5  "O  iO  iO  > 


'COCOCD(D!D(DO 


CO  CO  CD  CO  CO  CO  CO  CO  CO  CO  < 


CO  CO  CO  CO  CO  CO  CO  c 


)0O  t^coco  CO  < 


hmmihh 


1-1  ,* 


Is 

«<£ 

.-*  *> 
C3S 
fe  ft 

So 


ILLINOIS   STATE  GEOLOGICAL   SURVEY. 


Bull.   No.    22,   Plate  XXVII. 


A. 


A.  A  portion  of  the  Ohio  Oil  Company's   tank   farm,   Stoy,   111. 

B.  A  cleaning  rig. 


BLATCHLET]  OIL     STATISTICS.  169 

The  Princeton,  Indiana,  Sandoval  and  Carlyle,  Illinois  oils  are  above 
30°  B.  and  are  controlled  by  the  market  price  of  the  better  Illinois 
grades. 

Pipe- Line  Eras  and  Stocks  of  Illinois  Oil. 

The  annual  statistics  of  the  production  of  petroleum  in  Illinois  are 
compiled  by  Dr.  D.  T.  Day  of  the  IT.  S.  Geological  Survey  and  com- 
prise the  pipe-line  runs  of  the  Ohio  Oil  Company,  Tidewater  Pipe-line 
Company,  and  the  Indian  Eefining  Company,  and  the  tank-car  ship- 
ments of  the  Sun  Oil  Company,  Cornplanter  Eefining  Company,  Indian 
Refining  Company,  Missouri-Illinois  Oil  Company,  Central  Eefining 
Company,  W.  F.  Watson  of  Bridgeport,  Illinois,  and  Eogers  and  Dibble 
of  Oil  City,  Pa.  The  actual  production  of  oil  is  the  amount  which  has 
been  run  from  the  producers  tanks  into  the  tanks  of  the  transportation 
company,  whether  it  is  a  railroad  company  or  pipe-line,  and  from  thence 
discharged  through  general  pipe-lines  to  various  refineries.  The  ship- 
ments recorded  in  the  oil  journals  each  month  are  used  merely  as  a 
check  to  make  accuracy  more  certain.  The  federal  survey  has  in  con- 
templation the  collection  of  oil  and  gas  statistics  directly  from  the 
producer,  thus  placing  a  check  on  the  general  figures. 

summary  tables. 

The  total  amount  of  oil  produced  previous  to  1905,  when  the  main 
fields  were  opened  up,  is  almost  negligible  in  comparison  with  the 
present  annual  production.  The  following  brief  table  gives  the  yearly 
production  from  1889  to  1911  inclusive:1 

Annual  Production  of  Oil  From  Illinois  Fields,  1889-1911. 
Year.  Bbls. 

1889    1,460 

1890 900 

1891  675 

1892  521 

1893  400 

1894  300 

1895 200 

1896  250 

1897  500 

1898  360 

1899 360 

1900  200 

1901  250 

1902  200 

1903 0 

1904     0 

1905 181,084 

1906     4,397,050 

1907  24,281,973 

1908  33,686,238 

1909 30,898,339 

1910  33,143,362 

21911 31,317,038 

Grand    total    157,911,660 

i  Day,  D.  T.,  Mineral  Resources  of  the  U.  S.  for  1910,  Part  II,  U.  S.  Geol.  Survey,  1911.  p.  331. 
2  Day,  D.  T.,  Mineral  Resources  of  the  U.  S.,  calendar  year  1911,  advance  chapter,  1912,  p.  64. 


170 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


The  two  following  tables  present  the  ranks  of  the  various  petroleum- 
producing  states  for  the  years  1905-1910: 

Rank  of  petroleum-producing  States,  with  quantities  and  percentages  pro- 
duced by  each,  from  1905  to  1911,  in  barrels. 


State. 

Rank. 

Quantity. 

Percentage . 

1905.1 
California 

1 
2 
3 

1      < 

'            5 
6 

7 
8 

}      • 

10 
11 
12 
13 

}      » 

33, 427, 473 
28, 136, 189 
16,346,660 

12,013,495 

11,578,110 
10,964,247 
10,437,195 
8,910,416 

1,217,337 

1,117,582 
376, 238 
181,084 

8,454 

3,100 

24  81 

20  89 

Ohio 

12  13 

8  92 

8  59 

8.14 

7.75 

6  61 

.90 

83 

28 

Illinois 

14 

] 

i        M 

Missouri 

Total 

134,717,580 

100 .00 

1906.2 

)  : 

4 
5 
6 

7 
8 
9 
10 

}      » 

12 
13 

)  » 

33,098,598 

21,718,648 

14,787,763 

12,567,897 

10,256,893 

10,120,935 

9,077,528 

7,673,477 

4,397,050 

1,243,517 

1,213,548 

327,572 
7,000 

3,500 

26.17 

Indian  Territory 

17.17 

Oklahoma 

Ohio 

11 .69- 

9.9J 

8.11 

West  Virginia 

8.00 

7.18 

Indiana 

6.07 

•  3.47 

New  York 

.98 

.96 

.26 

] 

>■              .01 

J 

Total 

126,493,936 

100.00 

>-        1907.2 

i   ; 

3 

4 
5 
6 
7 
8 
9 
10 

}      » 

12 

i  :: 

45,933,649 

39,748,375 
24,281,973 
12,322,696 
12,207,448 
9,999,306 
9,095,296 
5,128,037 
5,000,221 
1,212,300 

820,844 

331, 851 

9,339 

4,000 

27.65 

23.93 

Illinois 

14.62 

7.42 

Ohio.                    

7.35 

6.02 

5.48 

Indiana 

3.09 

3.01 

.73 

.49 

.20 

Utah. 

) 

.0, 

J 

Total 

166,095,335 

100.00 

i  Griswold,  W.  T.,  Mineral  Resources  of  the  U.  S.f  or  1906,  U.  S.  Geol.  Survey,  1907,  p.  830. 
2  Day,  D.  T.,  Mineral  Resources  of  the  U.  S.  for  1907,  Part  II,  U.  S.  Geol.  Survey,  1908,  p.  348. 


ILLINOIS   STATE   GEOLOGICAL   SURVEY. 


Bull.   No.    22,   Plate   XXVIII. 


A    35,000-barrel    tank    fire. 


BLATCHLEY] 


OIL    STATISTICS. 
Table — Continued. 


171 


Oklahoma. 
California. 
Illinois 


Texas 

Ohio 

West  Virginia. 
Pennsylvania. 

Louisiana 

Indiana 

Kansas 

New  York 

Kentucky 

Colorado 

Wyoming 

Utah 

Missouri 

Michigan 


Total. 


California 

Oklahoma 

Illinois 

West  Virginia. 

Ohio 

Texas 

Pennsylvania. 

Louisiana 

Indiana 


New  York . 
Kentucky. 
Colorado.. 
Wyoming. 
Michigan.. 
Missouri.. 
Utah 


Total. 


California 

Oklahoma 

Illinois 

West  Virginia. 

Ohio 

Texas 

Pennsylvania. 

Louisiana 

Indiana 


New  York. 
Kentucky . 
Colorado.. 
Wyoming. 

Utah 

Michigan. . 
Missouri.. 

Total.. 


California 

Oklahoma 

Illinois 

Louisiana. 

West  Virginia. 

Texas 

Ohio 


1909.1 


1910.2 


1911.3 


1 

45,798,765  I 

25.65 

2 

44,854,737 

25.13 

S 

33,686,238 

18.87 

4 

11,206,464  , 

6.28 

5 

10,858,797  I 

6.08 

6 

9,523,176  | 

5.33 

7 

9,424,325 

5.28 

H 

5,788,874  1 

3.24 

9 

3,283,629  \ 

1.84 

10 

1,801,781  | 

1.01 

11 

1,160,128 

.65 

12 

727,767 

.41 

13 

379,653  | 

.21 

17, 775 
15,246 


178,527,355 


55,471,601 

47,859,218 

30,898,339 

10,745,092 

10,632,793 

9,534,467 

9,299,403 

3,059,531 

2,296,086 

1,263,764 

1, 134, 897 

639,861 

310,861 

25,806 


183,170,874 


73,010,560 

52,028,718 

33,143,362 

11,751,871 

9,916,370 

8,899,266 

8,794,662 

6,841,395 

2, 159, 725 

1,128,668 

1,053,838 

468, 774 

239, 794 

119, 045 


209,556,048 


81,134,391 
56,069,637 
31,317,038 
10,720,420 
9, 795, 464 
9, 526, 474 
8,817,112 


01 
.01 


100.00 


30.28 

26.13 

16.87 

5.87 

5.80 

5.21 

5.08 

1.67 

1.25 

.69 

.62 

.35 

.17 

.01 


100.00 


34.84 

24.83 

15.82 

5.61 

4.73 

4.25 

4.20 

3.26 

1.03 

.54 

.50 

.22 

.12 

05 


100.00 


36.80 
25.44 
4.21 
4.86 
4.44 
4.32 
4.0  J 


i  Day,  D.  T.,  Mineral  Resources  of  the  U.  S.  for  1909,  Part  II,  U.  S.  Geol.  Survey,  1911,  p.  304. 

2  Day,  D.  T.,  Mineral  Resources  of  the  U.  S.for  1910,  Part  II,  U.  S.  Geol.  Survey,  1911,  p.  329. 

3  Day,  D.  T.,  Mineral  Resources  of  the  U.  S.  for  1911,  advance  chapter,  1912,  U.  S.  Geol.  Survey,  p.  10. 


172  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 

Table — Concluded. 


State. 

Rank. 

Quantity. 

Percentage. 

1911. 

8 
9 
10 
11 
12 
13 
14 
15 
16 
17 

8, 248, 158 

1,695,289 

1,278,819 

952,515 

472,458 

226,926 

J            194,690 

J 

3.74 

77 

Indiana 

58 

43 

22 

Colorado 

.10 

Utah 

.09 

Total 

220,449,391 

100 .00 

Rank  of  petroleum-producing  States,  with  value  of  production  and  percentage 

of  each,  from  1905-1191. 


State. 


Rank. 


Value. 


Percentage . 


1905.  i 


Ohio 

West  Virginia. . . 
Pennsylvania  — 

Indiana 

California 

Texas 

Kansas 

Ind  an  Territory. 

Oklahoma 

Louisiana 

New  York 

Kentucky 

Tennessee 

Colorado 

Illinois 

Wyoming 

Michigan 

Missouri 


Total. 


1906.  i 


Ohio 

Pennsylvania. .. 
West  Virginia. . . 

Kansas 

Indian  Territory 

Oklahoma 

California 

Indiana 

Texas 

Louisiana 

Illinois 

New  York 

Kentucky 

Tennessee 

Colorado 

Wyoming 

Michigan 

Missouri 


Total. 


1907.  " 


Oklahoma 

Kansas 

Pennsylvania. 


$17, 
16, 
14, 
9, 


054,877 
132,631 
653, 278 
404, 909 
8, 201, 846 
7, 552, 262 

6, 546, 398 


,  601, 325 
557,630 

943, 211 

337, 606 
116,561 

54,865 


$84,157,399 


$16, 
16, 
16. 


997, 000 
596, 943 
170,  293 

, 615, 198 

, 553, 430 
, 770, 066 
, 565, 578 
557, 838 
,  274, 818 
995, 377 

031,629 

262,675 

53,890 


$92, 444, 735 


$18,478,658 
17, 579, 706 


Griswold,  W.  T.,  Mineral  Resources  of  the  U.  S.,  1906,  U.  S.  Geoi.  Survey,  1907,  p.  830. 
Day,  D.  T.,  Mineral  Resources  of  the  U.  S.  1907,  Part  II,  U.  S.  Geol.  Survey,  1908,  p.  349. 


20.27 
19.17 
17.41 
11.18 
9.74 
8.97 

7.78 

1.90 
1.85 

1.12 

.40 
.14 

.07 


100.00 


18.39 
17.95 
17.49 

10.40 

10.34 
7.32 
7.10 
3.85 
3.54 
2.16 

1.12 

.28 

.06 


100.00 


15.38 
14.64 


BLATCHLEY] 


OIL    STATISTICS. 
Table — Continued. 


173 


State. 

Rank. 

Value. 

Percentage. 

1907. 
Illinois 

3 
4 
5 
6 
7 
8 
9 
10 

}      » 

12 
] 

}      13 

J 

S16, 432, 947 
15, 852, 428 
14,769,888 
14, 699, 956 
10,401,863 
4,536,930 
4,063,033 
2, 127, 748 

862, 396 

272, 813 

28,383 

13.68 

13.20 

Ohio : 

12.30 

California 

12  24 

Texas 

8.66 

Indiana 

3.78 

Louisiana 

3.38 

New  York 

1.77 

Kentucky 

Tennessee 

.72 

Colorado 

23 

Utah 

"Wyoming 

Michigan 

.02 

Missouri 

Total 

5120,106,749 

100.00 

1908.1 
California 

1 

2 
3 
4 
5 
6 
7 
8 
9 
10 
11 
12 
13 

!   - 

J 

$23, 433, 502 

22,649,561 

17,694,843 

16,911,865 

16,881,194 

14, 178, 502 

6,700  708 

3, 503, 419 

3, 203, 883 

2,071,533 

746,695 

706,811 

346,403 

50,265 

18.15 

Illinois 

17.55 

Oklahoma 

13  71 

West  Virginia 

13.10 

Pennsylvania 

13  08 

Ohio 

10.98 

5.20 

Louisiana 

2  71 

Indiana 

2  48 

New  York 

1  60 

Kansas 

.58 

Kentucky 

Colorado 

27 

Missouri 

Wyoming 

.04 

Michigan 

Total 

$129,  079, 184 

100.00 

1 
2 
3 
4 
5 
6 
7 
8 
9 

11 
12 
13 
14" 
15 
16 
17 

$30, 756, 713 

19,788,864 

17,642,283 

17, 428, 990 

15, 424, 554 

13,225,377 

6,793,050 

2, 022, 449 

1,997,610 

1,878,217 

518, 299 

491,633 

318, 162 

\              42, 286 

23.97 

Illmois 

15  42 

W  est,  \  irgmia 

13.75 

Oklahoma 

13  58 

Pennsylvania 

12  02 

Ohio 

10  31 

5  30 

Louisiana 

1  58 

Indiana 

1  55 

New  York 

1  46 

40 

Kansas 

38 

Colorado 

.25 

Wyoming 

Missouri 

Michigan 

.03 

Utah 

$128,328,487 

100.00 

1910. 2 
California 

1 
2 
3 
4 
5 
6 
7 
8 
9 

$35, 749, 473 
19, 922, 660 
19,669,383 
15,720,184 
11,908,914 
10,651,568 
6, 605, 755 
3,574,069 
1, 568, 475 

27  95 

Oklahoma 

15  58 

15.38 

West  Virginia 

12.29 

9  31 

Ohio 

8  33 

5  16 

Louisiana 

2  80 

1.21 

i  Day,  D.  T.,  Mineral  Resources  of  the  U.  S.,  1909,  Part  II,  U.  S.  Geol.  Survey,  1911,  p  306. 
2  Day,  D  .T.,  Mineral  Resources  of  the  U.  S.,  1910,  Part  II,  U.  S.  Geol.  Survey,  1911,  p.  330. 


174  OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 

Table — Concluded. 


State. 


Rank. 


Value. 


Percentage . 


New  York. 
Kansas . . . 
Kentucky . 
Colorado.. 
Wyoming. 

Utah 

Michigan.. 
Missouri. . 


Total. 


1910. 


1911. 


California 

Oklahoma 

Illinois 

West  Virginia 

Pennsylvania 

Ohio 

Texas 

Louisiana 

New  York .«. 

Indiana 

Kansas 

Kentucky 

Colorado 

Wyoming 

Utah 

Missouri 

Michigan 


$1,414,688 
444,763 
324,684 
243, 402 

98, 330 


$127,896,328 


$38, 
26, 
19, 
12, 
10, 


719,080 
451,767 
734,339 
767, 293 
894, 074 
479, 542 
, 554, 552 
668,814 
248,950 
228,835 
608, 756 
328,614 
228, 104 

132, 032 


Total $134, 044, 752 


•1.11 
.35 

.25 
.20 

.08 


100.00 


28.89 

19.73 

14.72 

9.52 

8.13 

7.07 

4.89 

4.23 

.93 

.92 

.45 

.25 

.17 

.10 


100.00 


The  total  production  in  Illinois,  by  months,  for  the  last  six  years  is 
given  in  the  following  table:2 

Production  of  petroleum  in  Illinois,  1905-1911,  by  months,  in  bbls. 


Month. 


Year. 


1905. 


1906. 


1907. 


1908. 


1909. 


1910. 


1911.3 


January... 
February.. 

March 

April 

May 

June 

July 

August 

September. 
October. . . 
November. 
December. 


Total. 


6,521 
17,306 
23, 827 
26,586 
27,589 
34,611 
44,644 


181, 084 


55,680 
65, 208 
19, 352 
102, 862 
267, 746 
410,655 
610, 401 
778, 464 
722, 168 
463,819 
350,985 
549, 710 


4, 397, 050 


781, 812 
956,399 
1,547,323 
1,874,465 
2, 138, 918 
1,879,362 
2, 422, 192 
2,446,042 
2,605,663 
2,863,812 
2,510,146 
2,255,839 


24, 281, 973 


2,703,973 
2, 572, 115 
2,825,491 
3, 249, 690 
3, 223, 515 
3,081,848 
2,693,288 
2,808,667 
2,675,385 
2, 709, 913 
2,479,926 
2,662,427 


33, 686, 238 


2, 668, 607 
2,510,548 
2,  757, 794 
2. 562,  215 
2,829,277 
2, 670, 549 
2, 728, 857 
2,719,958 
1,902,197 
2, 560, 072 
2, 497, 847 
2,  490, 418 


30,898,339 


2,640,303 
2, 353, 684 
2, 865, 055 
2,776,800 
2, 860, 760 
2,746,620 
3, 029, 787 
3,007,151 
2,850,119 
2, 768, 750 
2,629,132 
2, 615, 201 


2,578,579 
2,373,229 
2,  790, 515 
2,560,963 
2,731,965 
2,634,521 
2,740,654 
2,770,946 
2,615,120 
2, 638, 927 
2,400,670 
2,480,949 


33,143,362 


31,317,038 


The  following  table  shows  the  value  of  Illinois  oil  produced  from 
1905-1911: 


i  Day,  D.  T.,  Mineral  Resources  of  the  U.  S.,  1911,  advance  chapter,  U.  S.  Geol.  Survey,  1912,  p.  10. 

2  Mineral  resources  of  the  U.  S.  for  1910,  Part  II,  U.  S.  Geol.  Survey,  1911,  p.  385. 

3  Day,  D.  T.,  Mineral  Resources  of  the  U.  S.  for  1911,  advance  chapter,  1912,  U.  S.  Geol.  Survey,  p.  64. 


BLATCHI.EY]  OIL    STATISTICS.  175 

Production  and  value  of  petroleum  in  Illinois,  1905-1911,  in  bbls. 


Year. 

Production. 

Total  value. 

Ohio  Oil  Co.        Other  lines. 

1 

Total  quantity. 

1905 

156, 503 
4,385,471 
23,733,790 
31,972,634 
27,640,773 
27, 751, 090 
25,987,480 

24,581 
11,579 
548, 183 
1,713,604 
3,257,566 
5,392,272 
5,329,558 

181,084 
4,397,050 
24, 281, 973 
33,686,238 
30,898,339 
33, 143, 362 
31,317,038 

$      116,561 

1906 

3,274,818 

1907 

16, 432, 947 

1908 

22, 649,  561 

1909 

19, 788, 864 

1910 

19, 669, 383 

1911 

19,734,339 

Total 

157,905,084 

$101,666,473 

The  following  table  presents  kind  and  amount  of  petroleum  pro- 
duced in  Illinois  from  1909  to  1911,  in  barrels:1 


Year. 

Light. 

Heavy. 

Total. 

1909 

28,049,468 
30, 444, 279 
29, 103, 220 

2,848,871 
2,699,083 
2,213,818 

30,898,339 
33,143,362 
31,317,038 

1910 

1911 

The  following  table  shows  the  pipe-line  runs  of  the  Ohio  Oil  Com- 
pany in  Illinois  from  1905-1911,  by  months,  in  barrels: 


Pipe-line  runs* 


Month. 


1905. 


1906. 


19.7. 


1909. 


1910. 


1911. 


January... 
February.. 

March 

April 

May 

June 

July 

August 

September. 
October... 
November. 
December. 


5,489 
9,208 
15,092 
19, 592 
26, 444 
34, 766 
45,912 


55, 680 
65, 208 
19, 352 
102, 862 
267, 746 
410, 655 
610, 401 
778, 464 
722, 168 
463,819 
350, 985 
538, 131 


Total 156,503 


4,385,471 


752, 671 
918, 620 
1, 494, 598 
1,823,025 
2,094,195 
1,830,634 
2,376,281 
2, 398, 895 
2, 560, 593 
2,818,032 
2,464,981 
2, 201, 265 


23, 733,  790 


2, 497, 359 
2, 464, 914 
2,  591, 911 
3, 089,  417 
3,084,816 
2, 965,  786 
2, 579, 977 
2.690,931 
2, 555, 871 
2, 582, 561 
2, 356, 386 
2,512,705 


31,972,634 


2, 494, 492 
2,358,198 
2, 568, 392 
2,388,309 
2, 536, 413 
2, 365, 956 
2, 413, 218 
2, 411, 483 
1,595,934 
2, 228, 269 
2,149,372 
2, 130, 737 


2,220,842 
1, 976, 637 
2,377,012 
2,306,336 
2,374,134 
2,274,501 
2,569,830 
2,528,532 
2,  409, 232 
2,334,659 
2,  211, 286 
2,168,089 


27, 640,  773 


27,751,090  25,987,480 


2,137,674 
1,968,429 
2,349,208 
2,138,500 
2, 264, 925 
2,177,280 
2,265,374 
2,312,973 
2,154,693 
2,172,457 
1,977,073 
2, 068, 894 


The  table  below  gives  the  gross  stocks  held  by  the  Ohio  Oil  Company, 
and  the  eastern  lines  operating  in"  Illinois  from  1907  to  1911,  by  months, 
in  barrels : 


i  Loc.  cit. 

»  Day,  D.  T.,  Mineral  Resources  of  the  U.  S.,  1910,  Part  II,  U.  S.  Geol.  Survey,  1911,  p.  385. 

*  Mineral  Resources  of  the  U.  S.,  1911,  advance  chapter,  1912,  IT.  S.  Geol.  Survev,  p.  65. 


176 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,      [bull.  NO.  22 


e 

i 

I 
I 

o 


o  6 

2« 


o  d 

o 


io  cm  o  ^  -"j*  o  ■ 


co~co~co~co~co~co~'"**'co~co*'cm*'cm" 


NfflOOHi 


•CM  C5CO  CM.-H 


THO«03lrtO>MNT-lrH(OC<5 


Mi-KONrtNHHOVOlN 

cones  co  &&$'■<&-&'■*?<?$  ofee" 


HNOOCOtOOO)MOH©CO 


CM  CM  <M  CM 


Ct>  Os  Oi  CT>  00  ■: 
CM  CM  CM  CM  CM  < 


g,, 


o- 

q  d 


He, 

Si  <n 


o- 

o  d 

O 


t^ 

Oh 

o  d 

2o 

o 

8881 


COMNiOOOOl-TOtOaoOCO 

ccccT^iwi^c<rco'-<i'*'coc<r<N~fcr 


~    X    r.OI'OC'tNtOOM 
N  ?D  O  N  S  N  Z   CO  CM  CO    •    -f 


i  O  CO  CC  C.  1^  M  OS  iO  CO  . 
co    -  -  —  ?  i  s.  r-  co  i  -  i 

*00lO00(OCDCOlOW 


lOOlONrJl-^COOOCCOm 

lONwooi-aa  -o  to 


i  tOCM  t^.  CM 


to  as  o>  cm  a>  cm  ! 

oa. 

CM~CM~CO~CM~CO~CO~0cTcm'''cM~CO~COS 


CM  as  CM  CO  <_    - 

HTJ>LflONlOO)N 

"lO^CMt^OOCMiO 


-s<  oo  co  •«  O  £-  co 

lO  t;  COCO  CM 


. .  oo  -&  a>  as  oo  to  < 

NffliOOCOHHtONH- 


O)  O  lO  O  1^  C  tD  N  l<:  c  iO  N 
CM  tO  t—  CM  I  -  LO  CO'  tO   >"-   r.  C  '' 

HOOJ^O^OINVCOOM 


■OiONOOHNl 


i  uo  to  oco 


■  00  N  X  N  iC  N  If  i.O  i— I 


CMCO-^iUOt^'XOOCMCO-^'O 


bS 


p-s 


3-gc3 


a  s  s  s 


"3  03  o,  c3  S  73  3  S1  O  O  a> 


GQ-g 

O.H 

raO 
®_ 

|S 

o  © 


is 

cS'S 


ILLINOIS   STATE   GEOLOGICAL   SURVEY. 


Bull.  No.   22.   Plate  XXXI. 


A. 


A.  A  gas  well. 

B.  A   gas   well   with    a    water   retainer. 


BLATCHLET] 


OIL    STATISTICS. 


177 


The  following  table  shows  the  quantity  of  petroleum  shipped  by  rail- 
road from  the  Illinois  oil  fields,  1906  to  1911,  by  months.  The  amounts 
were  estimated  by  Dr.  D.  T.  Day  of  the  U.  S.  Geological  Survey,  on  the 
basis  of  7.16  pounds  to  the  gallon  in  1906,  and  from  296.476  to  321.17 
pounds  to  the  barrel  in  1907  to  1911: 

Rail  shipments  of  oil  from  Illinois.  1906-1911,  by  months. 


Month. 


1907. 2 


1908. 3 


1910.  » 


1911.  s 


January.. , 
February . 
March . . . . 

April 

May 

June 

July 

August... 
September 
October... 
November 
December. 

Total. . 


60, 134 

51, 358 

16,009 

35, 539 

160, 121 

358, 039 

515, 956 

534,821 

368, 625 

162, 547 

48, 747 

30, 843 


8,701 


14, 
23, 
42, 
158, 
166, 
322, 
223, 
70, 
56, 
56, 


2,342,739 


1,210,019 


91, 807 

71. 170 
132, 300 
118,074 

84,  290 
122,317 
107,688 

70. 171 
83, 042 

102, 163 
138,147 
126.967 


1,  248, 136 


144,511 
111,407 
152, 056 
109, 872 
157, 783 
183,  432 
158, 642 
166,943 
173, 509 
200,067 
198, 044 
185, 166 


1,941,432 


220, 856 
217,917 
263, 056 
257,292 
283,  285 
285,095 
276,533 
277,317 
253,  788 
213,217 
287,  750 
234,819 


228,  404 
224,  856 
254, 927 
347, 530 
333, 324 
329, 621 
311,681 
297, 784 
238, 917 
292,004 
263, 627 
285,082 


3,070,925 


3,407,757 


1  Shipments  were  made  from  loading  racks  at  Bridgeport,  Oilfield  and  Stoy.  The  railroads  were  the 
Vandalia;  the  Baltimore  &  Ohio;  the  Cincinnati,  Hamilton  &  Dayton:  and  the  Indianapolis  Southern. 

2  Shipments  were  made  from  loading  racks  at  Duncansville,  Lawrenceville,  Stoy,  Robinson,  Bridge- 
port, Oilfield  and  Casey.  The  railroads  were  the  Vandalia;  the  Baltimore  &  Ohio;  the  Cincinnati,  Ham- 
ilton &  Dayton;  the  Indianapolis  Southern  and  the  Cleveland,  Cincinnati,  Chicago  &  St.  Louis. 

3  Shipments  were  made  from  Duncansville,  Lawrenceville,  Stoy,  Robinson,  Bridgeport,  Sparta  and 
Casey.  The  railroads  were  the  Vandalia;  the  Baltimore  &  Ohio;  the  Illinois  Southern;  the  Indianapolis 
Southern:  and  the  Cleveland,  Cincinnati,  Chicago  &  St.  Louis. 

4  Shipments  were  made  from  Duncansville,  Flat  Rock,  Lawrenceville,  Stoy,  Robinson,  Bridgeport. 
Casey,  and  Sparta,  the  same  railroads  shipping  in  1909  as  in  1908.  The  number  of  tank  cars  shipped  in 
1909  was  11,820. 

5  Shipments  were  made  from  Duncansville,  Flat  Rock,  Lawrenceville,  Stoy,  Sandoval,  Bridgeport, 
Casey  and  Sparta,  the  same  railroads  shipping  in  1910  as  in  1908  and  1909.  The  number  of  tank  cars 
shipped  in  1910  was  17,049. 

The  following  table  gives  the  statistics  of  field  operations  since  1905 : 


—12  G 


178 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


OS 

,CM  t>.^ 

•  CM  f- 

1—1 

30 

iO 

o 

CO 

© 

OS 

COIN 

co 

CO                         OS             CO 
CM 

i-HCN 

CO 

00 

CO 

OS 

•  i  - 

'«hoo^<n-h!ooohnohc<: 

:    8-      -,UB      ^    M 

1 

1 

.  30 

HOHN 
CO  .-1 

CO 

00 

O 

lO 

8 

t 

CO 

o 

CO 

8 

OS 

■o 

S.S8S 

co 

CO 

CD 

| 

CO 

> 

'43 

1 

o 

OS 

^icq      co 

i-l        CO 

COCO 
CO 

T 

CM 

o 

o 

OS 

00 

■a<oeo 
os 

00 
lO 

CO 

CO 

1 

-v 

C»00MINHC^MHH(ONH 

CO 
OS 

of 

1 

2S 

OS 

OOOhn 
00  CO 
OS 

00 
CO 

>o 

os 
o 

I 

OS 

LO  rf  OS  rH 
rr  cOCO^h 

CO 

US 

8 

1 

CO 

I- 

Ioosocn 

00  lO 

CO 

•«*< 

oT 

f 

OS 

>-H  O  t~-          00>-t 

U5?5f,HS 

>o 

O 

CO 

CO 

co 

o" 

OS 

t^cN 

uOOt^CMCNOOOSCNr^O 

— Ii-H                           CO                   CO 

(N                         CO 

rHCO 
CO 

OS 

CO 

i 

OS 

s 

tMCOCOcOCOOOTfiOSCSCOCMIMCO 
rHOscO             <-i<M.              MH        CO 

co" 

00 

o 

OS 

88 

M 

OS  CNCNOS 

CNJ  -<Cfl 

CO 

of 

CO 

w 

co" 

1 

•i 

OONiO 
00  »H 

of 

OS 
CO 

00 

88 

OS 

2 

co 

1OO00N 
CO  CO  lO  CO 

CO 

§ 

CO 

s 

co" 

1 

o 
O 

e 

c 

pq 

-if 
r 

5 

2 

i. 

3 
o 

c 
1 

T3 

1 

S  6 

OS 

c 
o 
-/ 

1 

a 

c 
c 

J 

e! 

- 

a 
1 

c 

1 

V 

2 
C 

c3 

o 
«c 
p 

ci 

P4 

a 
p 

X 

a 
c 

C 
/ 

£ 

1 

c 

•^  O  SsflM 

r<£jio^ 

.   S   M    « 
^s  ^5    CP    CP 

bTa.3.5 
£  °  a  a 


BLATCHLEY] 


OIL    STATISTICS. 


179 


CD 

J 

1 

*i 

o 
t- 

1 
® 
S? 

> 

< 

© 

cqt>- 

COO 

oo 

■  ^ 

!© 

© 
CO 

CO 

o 

© 

o  oo 

lOCN 
CNCN 

icNOO^ 
.  ©  t^tN 

qt>. 

OCN 

T-l     © 

CO 

© 

3 

© 

!© 

■lOiOMOOHiOOONiOO 

'Olfl^OMNHlOONNCO 
•  r-t  CN  CM                   CO       H  CO  t>- 

CO 

co 

1 

.'co 

CO 

ri 

1  eo  io  oo  ■<* 

•  O  CO  ©  CO 

•  r- I  CN 

CO 

© 

d 

CN 

© 

CN 

I-* 

o 
© 

© 
n 

©CN©  !>• 

NtOO 

CN 

© 

CO 

CO 

CO 

s 

w 

8 

no  i-j  os  oo 

CO  CN 

© 
S 

00 

* 

© 

Total  initial  production. 

© 

811 

11,681 

10 

9,802 

125 

©- 

rr 

CO 

© 
© 

CO 

© 

© 

3S. 

00 

lO  <M  (M 

O00  CO 

CO  ^H 

co" 
CN 

©uo 
© 

© 
so 

ro~ 

»c 

© 

co" 
© 

1 

3! I 

lOOiOOOCOOCOLOOcOiCCO 
©  r-  uO  r-<         UO  uo         ,-1  !N  ->J< 
COO                   O             CN  .-1 

© 
©" 

00 

00 

o 

© 

CO 

© 
to" 

122 

46, 694 

303 

45 

> 

§ 

© 

CO 

© 
oo" 

o 

© 

00 

re 

o 

CM 

314 

84, 163 

3,612 

118 

CO 

— 

00 
CN 

CO 

© 
©" 

CO 

I 

-.o 
rr 

co 

279 
59,  204 
15,115 

101 

1 

1> 

3 

CN 

© 

co" 

1 
o 
O 

1 

5 

= 

£ 

a 

- 
z 

5 
3 

c- 

t 

- 
a 

— 

z 

- 
— 

i 
P 

a 

= 

OS 

= 
o 

8 

i 

/ 

- 

1 

— 

- 

C 
z 
~z 

i 

1 

- 
p 

T 

c, 
/ 

0 

z 
c- 

180 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


3 

o 

CO  00  Tt<  -H  OS  Tf> 

oo  oo  r- io  co  co 

CM  OS  lOH  i-H  CO 

co^Tj^co'co'c^T-r 

o 
© 

ft 

■*  Tf  00  CO  CO  00 
lf3  M  N  N  CO  O 
COCOCMH  r-H^H 

> 

o 

COO  CO  CO  r- OS 
t~-  CO  !>■  CM  t>-  CM 

CO -H  CM  OS  rH  H 

O 

(OMOCNXN 

"Ocoa^ao 

^  CO  CM  CS|  —t  ri 

P. 

CO 

OS  O  t»<  CM  •>*<  00 
■"J"  O  >*  00  CO  CO 

tub 

3 

-4 

CO  i-H  t~-  CO  >0  CO 

as co^ o co  •«< 

■f  •*  T(i  CO  CM  rt 

CO  CM  t~-  r»«  tx  CM 
■>»<  iO  rfi  CO  ^H  rt 

© 

a 
3 

CO  CO  CO  CO  CM  i-h 

03 
3 

CO  CO  Tt<  -H  CM  t- 

iCOltONOiH 
CS  tt  CM  CO  ^H^H 

ft 
<1 

00  t^  t-CO  t-H 

O  CO  Os  O  iC  00 
HMtHNH 

C3 

^  t^-CO00^H 
COr-lCM^H 

P 

CJ 

tONTjiooca 

•O  to  CM  iC  00 
CO.-I  CN^H 

c3 
l-S 

CO  CO  CO  t— *  Tf* 

•o  o  ^h  i-)  o 

(MCOOlr-lrH 

3 

- 
9 

E 

3 

5 

5 

ro 

~^ 

OS 

>H 

80 

•r» 

o 

* 

~ 

ft 

Kl 

e» 

>, 

*« 

d> 

> 

5 

o 

CO 

o 

Q3 

co 

o 

t3 

==>. 

l_J* 

5^ 

1-1 

■« 

3 

o 
Eh 

O  CO  iO  00  00  iO 
»(NiO>OCOO 
-<J<  t^  io  »o  ^  CO 

i 

-HCM  CM  CM  GO  00 

CO  lO  1«  CO  CO  r-( 

o 

CO  00  ■*  tQ  CO  CM 

o 

O 

NNH00ON 
Tfi  00  lO  ■»  CO  ^H 

1 
OQ 

oscmoso  oooo 

CO  CO  •<*>  lO  -cr  CO 

< 

00  -cmO  >0  Th  CM 

>> 

3 

OS  CM  iO  OM  CO 
CO  I-  CO  tO  •*  CM 

I 

~H  IO  Tf  CO  O  CO 
-<J<  I>.  iO  iO  iO  Ti 

03 

r^  ■*  io  io  co  co 

CO  CO  CO  -^"Cf  CO 

Pi 

«4 

OOM00HO 

cm  -en  co  co  ■*>  r-i 

o 

c3 

CO  CO  ">r  CM -h 

ft 

igSSSS 

a" 

03 

-*l  IO  Tf<  i-H  CM 

i 

s 

3 

l 

3 

5 

5 

1   tdO  CdO 

TlO  i— i 

Q©  a> 

Q3S 


CO  CO  iO  iO  . 
HOI  l^CMc 


i^cxrco""t>^t-^c<r? 


I  O  CM  00  CM  CO 
I  00  -tfi  CM  CO  CM 
i  t^  CM  CO  CO  00 


o  a>  co  os  oo  io 


14,03< 
8,15' 
6,09 
8,90< 

10, 13; 
4,78! 

io  t^  oo  ■*  as  co 

OCOtCNHN 

!>•  as  oo  co  -<f  "O 

CM  O  CM  i-H  CM  00 

co  -n  cm  co  ■"*!  r^ 

-<f  CM  CO  CO  O  iO 


(NH00  00ON 


CNJ  lO  iO  O  ( 


io  o  oi  as  co  as 


H00  00ON00 

r^  oo  cj>  as  as  >o 


i-i  CO  CO  CO  O  i-h 

oo"~co~cot>T'ooic' 


l  00  CO  CO  00 
i  CM  CM  ■*  iO 


CCrt-jiiONlfl 


CM  CO  00  CO  a> 

OJCOrHOftO 

WHOiOOl 


NoimocN 


as  co  •*  co  co 


M^OHN 
CO  T1  CO  CO  t^ 

■*hOM!C 


as  co  io  io  io 


BLatchley]  NATURAL    GAS. 

Petroleum  field  report  in  1910,  by  counties. 


181 


Wells. 

Acreage. 

County. 

Productive, 
Dec.  31. 

Abandoned 

Drilling, 
Dec.  31. 

Fee. 

Lease. 

Total. 

Clark 

2,341 

67 

6,652 

677 

6 

124 

1 

217 

4 

1 

1,065 
140 
913 

58,515 

575 

102,737 

6,221 

80 

59, 580 
715 

Coles 

15 

103, 650 

6,221 

610 

Edgar 

530 

Jersey 

Lawrence 

2,411 

38 

30 
1 

329 

80, 615 
23,793 
11, 486 
35, 920 
493 
84, 760 

80, 944 
23,  793 

Macoupin.  . 

11,486 

Marion 

12 
5 

4 

407 

35, 920 
900 

Randolph 

84, 760 

Total 

12,171 

385 

50 

3,384 

405, 195 

408, 579 

On  January  1,  1912,  it  was  estimated  that  19,982  wells  had  been 
drilled  in  Illinois.  Of  these  3,  152  or  15.7  per  cent  were  barren.  There 
were  84  wells  abandoned  in  1910  and  198  in  1911.  The  abandonment  of 
wells  in  the  shallow  fields  has  been  under  way  since  1909  and  is  gradu- 
ally growing  as  the  sands  are  exhausted.  Unless  new  wells  from  deeper 
pay  sands  or  the  extension  of  portions  of  the  area  are  developed  this 
field  will  probably  be  completely  abandoned  by  the  close  of  1913.  The 
deeper  field  of  Crawford  county  is  showing  a  decline,  but  its  life  will 
be  much  longer. 

NATURAL  GAS  IN  ILLINOIS. 

Illinois  produces  a  very  small  amount  of  natural  gas  in  proportion  to 
the  immense  quantities  of  petroleum.  Her  rank  is  eighth  among  gas 
producing  states  with  the  following  preceding  her  in  order:  1,  West 
Virginia;  2,  Pennsylvania;  3,  Ohio;  4,  Kansas;  5,  Oklahoma;  6,  New 
York;  7,  Indiana.  The  principal  gas  areas  lie  within  the  oil  fields  and 
the  supply  is  used,  chiefly,  for  field  operations.  Gas  is  used  for  do- 
mestic purposes  in  the  towns  within  the  oil  belt  and  in  several  others 
near  the  fields.  Gas  is  sold  in  Lawrenceville,  Bridgeport,  Pinkstafr, 
Birds,  Flat  Rock,  Oblong,  Palestine,  Robinson,  New  Hebron,  Porterville, 
Stoy,  Hutsonville,  Annapolis,  Casey,  Westfield  and  Martinsville,  all 
being  in  or  near  the  oil  fields.  Outside  towns,  such  as  Marshall,  Vin- 
cennes,  Indiana,  Olney,  and  Sumner,  are  connected  by  direct  mains  with 
the  fields.  The  majority  of  active  oil  wells  produce  small  amounts  of 
gas,  which  is  collected  in  gas  tanks  on  each  lease.  There  are,  however, 
several  areas  within  the  fields  that  yield  high  pressure  gas  wells,  and 
these  serve  the  commercial  demand  for  the  fuel.  (See  PL  XXXI.) 
Such  areas  lie  near  Bellair,  Hardinville  in  Honey  Creek  township,  and 
north  of  Bridgeport.  The  gas  comes,  seemingly,  in  each  case,  from 
raised  portions  of  the  oil  horizon.  The  following  brief  table  shows  the 
approximate  depths  of  gas  sands  and  the  accompanying  pressures: 


182  OIL  FIELDS  OF  CRAWFORD  AND  LAWEENCE  COUNTIES,    [bull.  no.  22 

List  of  gas-sands  in  Illinois  fields,  ivith  depths  and  gas  pressures. 


County. 

Depth  in  feet. 

Pressure 
in  pounds  per  square  inch. 

1908. 

1910. 

105-330 
80-130 
250-550 
500-1000 
500-575 
94-120 
265-600 
900-1850 
175-280 
100-893 

0-30 

0-23 

Champaign 

15-32 

Clark 

65-100 
25-400 
15-35 

35-45 

20-225 

DeWitt... 

25-50 

75-127 

500-600 

200-750 

Lee 

18-28 

Pike 

3-10 

4-10 

Natural  gas  was  found  at  a  depth  of  1,528  feet  in  Marion  county 
during  1909-1910,  at  the  time  the  Sandoval  field  was  opened  up.  The 
original  pressure  was  about  370  pounds  to  the  square  inch.  Several 
wells  adjoining  the  first  one  developed  also  produce  gas  at  high  pressures 
and  the  product  of  all  of  them  is  used  for  field  operations  and  for 
domestic  use  in  Sandoval. 

A  new  gas  area  was  tapped  early  in  the  year  1910,  near  Greenville, 
Bond  county.  The  sand  is  found  between  950  and  1,000  feet  and  is 
correlated  with  the  Benoist  sand  of  Sandoval  and  the  Kirkwood  sand 
of  Lawrence  county.  Three  wells  yielded  from  1,250,000  to  2,000,000 
cubic  feet  of  gas  daily.  Several  light-pressure  gas  wells  were  drilled 
near  Jacksonville,  Morgan  county,  during  the  year  1910.  The  yield 
came  from  a  sand  overlying  the  St.  Louis  limestone,  at  a  depth  of  about 
300  feet.  The  gas  is  odorless,  colorless,  and  burns  with  a  very  hot, 
blue  flame. 

A  gas  area  similar  to  the  Jacksonville  field  was  tapped  in  1908,  near 
Carlinville.  Good  pressures  were  secured.  A  gas,  called  "drift  gas," 
has  been  obtained  from  the  Pleistocene  deposits  over  portions  of  northern- 
central  Illinois  and  used  for  the  past  25  years.  The  pressure  is  usually 
slight  and  the  lives  of  the  individual  wells  are  short.  The  depths, 
from  which  the  gas  comes,  vary  from  50  to  250  feet.  Wells  of  this 
type  have  been  drilled  near  Champaign,  Princeton,  Colchester,  Wapella, 
Heyworth  and  elsewhere. 

The  following  table  records  the  natural  gas  development  in  Illinois 
from  1906-1910,  according  to  B.  Hill:1 

Record  of  natural  gas  industry  in  Illinois,  1906-1910. 


Gas  produced. 

Gas  consumed. 

Wells. 

Year. 

Number 
of 
prod- 
ucers. 

Value. 

Number  of  consumers. 

Value. 

Drilled. 

Prod- 
uctive 

Domestic. 

Industrial. 

Gas. 

Dry. 

Dec.  31, 
1910. 

1906 

66 
128 
185 
194 
207 

$  87,211 
143,577 
446,077 
644, 401 
613, 642 

1,429 
2,126 
27,377 
28,458 
210, 109 

2 

61 

2204 

2518 

2479 

$  87, 211 
143,577 
446,077 
644,401 
613,642 

200 

1907 

94 
121 
56 

64 

41 
42 
11 
31 

283 

1908 

400 

1909 

414 

1910 

435 

i  B.  Hill,  Natural  Gas,  Mineral  Resources,  U.  S.  for  1910,  U.  S.  Geol.  Survey,  1911,  p.  317. 
2  Includes  number  of  consumers  and  value  of  gas  consumed  in  Vincennes,  Indiana. 


BLATCHLET] 


NATURAL   GAS   STATISTICS. 


183 


The  following  table  prepared  by  Mr.  Hill1  shows  the  total  estimated 
value  of  natural  gas  in  Illinois  from  1885  to  1910,  inclusive : 

Production  of  natural  gas  in  Illinois,  1885-1910. 


Year. 

Value. 

1885 _ 

$    1,200 

1886 

4  000 

1887 

1888 

1889 

10,615 
6,000 
6,000 
12,988 
14,000 
15,000 
7,500 
6,375 
5,000 

1890 

1891 

1892 

1893...              

1894...                         

1895...                                

1896...                  

1897 

1898 

2,498 
2,067 
1,700 

1899 

1900 

1901 

1,825 

1902 

1,844 

1903 

3,310 
4,745 

1904 

1905 

7,223 
87,  211 

1906 

1907 

143, 577 
446, 077 
644, 401 

1909... 

613,642 

» Idem,  pp.  300-301. 


184 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


i>.  — 

IN 

t-O-f 

O  TO 

«•*« 

«#■*•  1-H 

TOO 

*c5 

^ 

> 

0 

O^CO 

CO  o 

WtOw 

03 
O 

i*d 

00  t"-  Ci 

Eh 

. 

£g& 

■  © 

00CCCN 

§^ 

00  CN'cO 

t^  t^  CN 

3    I  £ 

OirfN 

§i 

toc'o 

+3 

00  CO  1-2 
CNOCN 

2 

L0  05CO 

"3 

> 

CM  CO  CO 
9% 

-d 

CD 

B 

2 

fl 

T   LO  «H 

'C 

to  O 

o  m  SO 

i 

CO 

!*« 

o 
o 

►d 

°£ 

3 

o 

fl 

a* 

r^  ~.  CTi 

CN  CO  CN 

,  £ 

OtCl 

3      «-• 

oo  cn  i-^ 

(MOO 

cr.  cn  t 

or* 

CO  tviO 

** 

C3  00  t^ 

lOHN 

00  CO  CO 

aj 

t'oo'oO 

O-rf^ 

-HCN  CN 

03 

■    a& 

> 

.2 

fl 

toioa 

"-*- 

to  O 

00C1--H 

CD 

a 

o 

lae 

T-H  i-(  CN 

°§3 

Q 

ft 

NHt- 

3 
i    © 

>OCN  i-O 

CNTO 

flg 

o'oo 

0<MCN 

<2*T 

t-TrHt-J" 

*" 

f  MO 

OhN 

B  "3 

(NOT 

1 

a -is 

0) 

s 

I 

_o 

NCCO) 

o 

CO 

COT  i-l- 

O 

© 

a 

o 

ft 

t>Too  o 

LO  T  t> 

22S 

ber  of 
pro- 
ducers 
having 

gas 
wells. 

i- 

:    l 

e4 

e 

>i 

« 

~ 

d 

CT>OiS 

1         i— 

BLATCHLET]  APPENDIX     IXDEX.  185 


APPENDIX— TABLES  OF   WELL  DATA. 


IXDEX    TO    TABLES. 

Pages 

From  To 

Crawford  county    , .  186  283 

Honey  Creek  township   186  196 

Martin  township 197  238 

Oblong  township    239  277 

Robinson  township    277  283 

Lawrence  county   283  436 

Bridgeport,  township    283  331 

Christy  township    331  332 

Dennison  township    332  364 

Lawrence  township 364  380 

Lukin  township    381 

Petty  township    ' 382  436 


186 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


"O     "3     "3 

:  a  :  3  :  c 

.  o    •  o    •  o 

j  ft  ;  &  ;  a 
IS  :§  :g 


:s 


»    'a? 


©£  oTfc  wfc  .-S    - 
^73  03  ft<3  ft 
■  WO      O 


^2 


03  03        °3 


•spjjBq— jonpoad  iBprai 


Q     Ofl 


■j98j— mdapiBioj, 


■j99j— mdapno 


sa 

o 

v. 

o 
to 


■%9QJ — aUBjd 

rany?p  8AoqB  apnji^y 


•180J— I8A8] 

B9S   Avojaq    gpnij^Y 


pa}i3j;8U9d  ssanjtojqx 


•;9aj— doj  oj  qjdea 


-1    .£PQ   IpfiOq 


T.  C:  ~  ~  T.  c~. 


/  — 

t-H  ^ 


§    5 


^hO^hOOOOO 


-I.SOOCDHM 


!N  <*         <M  «<*  -T  CC  ■ 


.D^^iiOOOO 

o  o  o  cd'O'C'd 

tftftftf  :  :  :  : 


Z2£ 


§28    ' 


iOO-hO  < 


■*P5^      WffnT' 


lO  00  O         TfOOONNN 


.3  >..H 

,Q  03,Q 
0£  o 
P3o2pH 


,©,© 

o  o 


-S  2-5,2 

3  >3  OT3 


C  OS 


*       2 


t:te 

03  O 


,_J  ,_i  c 

2  ©  i-H  ■**<  C<J  »0  eO     .     .  '""' 

rt~  °  £   2oc66d°£  © 

£  3  3."   ©  <»  aTaT  oTo"  2£  3~ 

*  3  3.-oooooo-3  3 

03  03  ^    3'CC  i-'C'C  ^  S  ^ 

§  §  ^.  -^  ft  ft  ft  ft  ft  ^M  a 


°  2 

2    . 

3     § 


s  «« 


te'S 


-5      -= 

3        -3 


~—     ^  o  o  0)  o  fl)  ffi 
•3         S3  ?3  S3. 5Q  Jd  ."£.  So 
"©  c3  03  c3  03  o3,£  c3 


s? 


& 

is  °3 

,3 

s 

P3 

•-    3,3^,3,3,3^  « 

s 

« 

0) 

P3 

(M 

(M     X  T  O  »  N  50  rt  N 

<N 

ro 

o    . 

■  -  o 

"2 


2  i  2*02 


BLATCHLET] 


TABLES    OF    WELL    DATA. 


187 


- 
p 
- 

■r 
■s 

r 
C 

P 
r 
or 

5 

? 

r 

E 
c 
s. 

a 
I 

8 

1 

co 

2 

H 

o 
© 

w 

a 

s 
is 

3 

Gas,  860  feet 

Gas,  885  feet 

Gas,  930  feet 

Gas.  888  feet 

05   ® 
«£«£ 

mo 

00  00 

r/T  co" 
03  03 

oo 

J. 
c 

C3 

© 

CO 

GO 

a" 

o 

!!> 

3«g 

_ 

as 

■2 

CN 

1 

s 

c 
1 

CN 

'- 
OS 

z 

0 

3 
CO 

CO 

73 

i 
a 

w 

'o 

u 

Pi 
Pi 

3 

1 

f 

1 

c- 
c 

COO 

.-  ~  ~ 

0 

CO 

oo  oo  co 

O  C  i  OS  C  -r 

,— 1  i— 1          NH 

— 

00 

O  O 
Oi<N 

gg 

oo  io 

CO  r-< 

o 

o 

(H 

ft 

ft 

- 

> 

n 

i  - 

3B 

CO 

s 

CO 
CO 

iO  o 

a)© 

ooo 

3£ 

O5  00 

5 

re 

O 

r 

ex 

-z 
X 

x 

•r 
- 

OJNtONtO 
GO  00  00  00  00 

7 

CN0C 

lOCNOMNNtO 


HhOHONNHHfflffii 

t-hOOOi-hOOi-hOO- 


cOi-<oo 

2Sg 


I-H  Ol-HrH© 


t~-  CO  CO  CO  r-  C5  ■ 

JNOVN(NO)( 

00CO-^lT}'lOCO'*iTriCO-^"»iCO'3<,V1' 


'co-w-^co-^eo'^rcococo' 


NONKl> 
00  CO  l«iO  < 
CO  ■*  coco  • 


— (  CO  CO  t-<  CN  CN  CO  CN 


©  lO      'COCO      'OM0)«e00»H00OVOO«3Ol 
tji  t«       .CNCN       .CNCN.-H.-H  (NHHKMVHMHrt 


1-H  t}H>  CO  O 


iO  CO  ■*  ffl  iO  00  IN 


ioooooo 


CO  X  X  s  o 


LO^^iOiOLOCNiOlOOCNOO-^r^OOOCOCOCN' 
a^WOJMiOXNOOi-'NOiNlONlOCecOMVHlOCCI 
OS  Ol  GO  00  00  0C  000000500000000GOG000000000050COOI 


<Ni-H 

ii 

to  -y; 

PI  p 
:ph£ 


!CN 

<N^h 

CNCO 

i-H  CN  i-(  CN      In'h      I  .-! 

:  pi 

.  o 

CO 

:  c 
:ph 

c 

c 
— 

> 

r 
i- 

X 

P  PI 

o  o 

CO    CO 

>9  9 

o  o 

Pnpw 

> 

T 

X 

o  o 

CO    CO 

.9.5  > 

,0,0    OS 

O   C£ 

P-Wx 

PI 
o 

a 

'3  = 

> 
r 

•7 

Robinson 
Robinson 
Robinson 
Robinson 

Stray 

Robinson- 
Robinson- 
Stray.... 
Robinson- 
Strav 

Pi 
o 

CO 

p 

3  c 

c  — 

Ph 

c 

:phP4 


tf  : 


p 
■2  2  3 

:phP3 


CO  Tfi         CM  CO  i-H       .CO 


;  i 


Pntftf  :pj 


—I    o    cj    r-o 


00  t^      1^.      r-H  CO      r^ 

io      t^    t^    go      t^    t- 


NN00     00         t~-t^r^         t^t^lOCOLO< 


CO      O     OS 


CO     ^     <-OCM 


y 

CO 

o 

CN 

CO 

if: 

io    o    t>      go    ejs* 


Z22Z^^        ^^^^^    ^g^g    g      g    g    g      g    g^    g    £££ 


o    o 


§  S  IS  §§     g      §    cc  cq  pa 


>»   >>fl  p  p    P 

O       O   <0   &    <&       03 

pa  pa^bdW  W 


p    p    p 

0)       0)       CB 

WWW 


+J-  ^-p    p    p  q  p 
pi    p|  9    p    3  p  p 

0)       ©   03       03       03    03   03 

w  w§  s sss 


^  55  jz; 


w  Ph     Ph  Ch  Ph 


_ 

2 

■~ 

o  o 

o 

— 

— 

-r 

T!-C 

— 

~ 

-d 

T! 

73  T3 

— 

- 

M 

^ 

Pnpi 

— 

H    tH    tH      H 

-h     CN     CO        <* 


03  O  O  O      O 

£333  3 

E-iOOO   O 

1OCON00      OS 


AAA 
O    O    O 


o    o 


£  *  t* 


073^3737373         '©'©'         "©    "©"© 

as  2  S2S     §  §     S  cl  § 

OPh    Ph    PhPhPh        WW        WWW 


188 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


•siaojeq— ;onpoad  i^rai 


•%q&1— qidop  no 


'loej— T^dep  pnoj, 


B8S    MOjaq   apn^ppv" 


pa^Jiatrad  ssanjpiqj, 


•paj— doq.  o;  qidaa 


m<5  ©  >.2«£ 


c?o 


cu1^ 
CO 


00  00  00  00 


p 


^00< 


up. 


CO 


■s.§ 


*£ 


3    CJ 


s"3 


A.SP 


00!NMOiO»0)1iWO(»HCDHONMCCHLOMO 
T-HOi-lOrHOl— lOi— I  O  T-H  O  f-  >— tOOi-HOr-Hi-Hl-Hr-li— I 


Mfco^cofco^co-<*ico-'ct<t-»co-<i<-'cticoTj<cococococo 


'irjffloOMWOiOW 


05  CO  t—  05  CO 
..M3N1C   !C   EC 

00000000000000OJ0005000KN0005C500O0000000000 


NMi-iCNrHCOiHCNrtCO 

oooooooooo 

a  a  s  a  a " ' 


,3  3  2  3  lo  2  3  3  3  3 
oooooooooo 


,0,0, 


;  iH  tN  CO  1-H  CN  r-4  <N  ,-i  <m"  — 

'.flicjpiaflflflflc: 
.oooooooooo 

,c/3c/3<z>coc»tMC/!OTC/:(/: 

•  3  3.3  5.3  5  3  3  9  5 
:  3  3  3  3  3333  3  3 

•oooooooooo 


t^-  r^  co  co  r^  c: 

CO  CO  CO  f  CO  f 


SOS 
O  o  C 

.3  3. 3 
2  £  £  3  3  2 
o'd'o  o  o  c 


t^      r-      oo 


00        CO     <Ji 


'i-H      —I      00  CN 


£  £   £     £   £ 


OO^^SS^fe 


X'  OHO  •*!  t-l 

dodo  d 

+j>    T3r0'0',d  "C 

K    o  o  o  o  o 

&n  pQpqpqpq  pq 


o  o 

WW 


rt    &    P3 


tf  o 


c3  C3  c3  c3 
Cf    CD   <0   <D 

££££ 

o  o  o  c 


.2  UOOO 

?  "c3"c3rt«  C 

P  HH&hEh  O   PC 

lO  HCNM^f  i-0     cot- 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


189 


1i 

Sis 


C3"c3 


o  oi 

A  o  — 

-Jim 


P2 


o  c  o  o  o 

re  iO  us  10  O 

_  ^H  rt  CO 


re  55  cm 

ooo 


oc  i  -  re  O  i  -  —  re 
— <  cm  ce  re  cm  re  re 

CO  ooooo 


CNCOXON      • 

■  o  o  o  o  o  —  o     ■ 

1  O  O  O  C  C  O  O      • 


o  d  o     -o -<  ce 


c  oo 
—  cm 

o  o 


CM  CM  ^  io  l^  CM  to  i 


K  N  C.  C  -  '/  M  ' 


lOOO^- 


i"  /  c:  r.  s  5  '/  I-  o  r» 

o  o  o  o  —  o  O  O  O  O 


re  co^r-  tt 


o  cm      xxcjlc  re  ■: 
02  r-      t^  ci  cm  ce  re  ( 


ac  —  CI-XH  IO 


ONWrtL'SCMNKCi 


o  o  cc  i.e  o  —  t-  re  o  >e 


i  O  O  r~  CM  : 


cm  re  re  re  re  re  cm  ce  cm  to  cm 


BO  O  C  —  —  I  -  3C 


c  cm  -o  -r  i>  o  t»  t—  os  w 


goo 

CM  re  t~ 
r-  -  O 


CM  Hi  t>-  X) 

ClGCiCi 


C  cr  cc  O  t~  re  re  to  r-  t-  ■ 


HNCCKIN 


»io      oncc.c  c  c  c  c.r  ;  /  c.  r  r.  ^jc.khkoc  io 
O  O      ooooooooo.  oooo.  occo.  ooocaosoa 


O  O  O  Ci  O  O  O  ~  O  O 


1    = 


CM 

■7 

= 
C 
or 

i 

>  CC' 

;«  : 


,CM*H 

:  c  c 

o  o 

C/l    CO 

:  n  g 

!   c   C 

:p3« 


>-o  .2 


2  o c  coco  o  c  d 

C  v'C'S'S'S'S'fl'C'C 

as::::::::: 


!e  j£  S 


:  io  io  uo  ue  io  «3  io 


o  o  o 
t^  t^-  r- 

io  m  »o 


II: 


I  CM  IO        CC  rt  lC  -  C  re  C  N  l-5  M  ■* 

•  r~  to      lcnz  i^  x  v.  o.  to  f~  r-  io 

l»C  iO        IO  C  c  i-C  c  c  lC  lCj  iC  IC  o 


i  $ 

C3      O 

■3    2 


„   o 


5   £ 


c  o 


iNn'*<oMoeiH 
Nxoo'o'dddoodo1 


o  o  o  c 

ZZ2Z 


.•fcfcZfcfcfcZfcZfc 


CO  CM 'T  tO  t^ 

6  d  d  d  o  o' 


ccocoooo 


XXXXXXXXXXj*~f«"^;£ 
IcSrtrccSctctrJrScSre"^®®®^ 


Z2Z^ZZ^^^^^ 


-r*  -c^  -r<  tJCrjOCJCcXSXcXSXU) 
ss2c»a>oocDt»e)© 


!£££: 


;£££ 


iimi 

J  J  J  J  _J  J 


CvCyC;C;wCcCwl.^-^DCOfli 

C3      22SS22SCCCqCECCCc3c3cS03c8c3 


cccoccco 


'G  cc  c=  tf  tf .^f.Hf.Sf.^.rf.Bf 
2  -  -  'S  'S  'S  '3  "S  'S  'S  *e3 


ixxxxttHWt 


WjjjjjGCwtoc;     ccaautccocoo 


i  cm  ce  Tf<  io      HNw»io-^'/.cr.c 


3235    I      Z     X 


190 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siaxreq— :pnpojd  repnii 


•}88j— qidap  ib^oj, 


ill 


CO  CM 

CO  CO 

oo 


o? 


cr 


0? 


Sop 


*s  o  o  o 
Cr 


CO  CM  C5  CM 

■*  co  eo  ui 

oooo 


•}88j— mdap  no 


©OOOOOOOSOOX 


iQOiOOl 


(DNOOOONMOHOIOO 
OOiOOOOOO©©© 


nin^p  8AoqB  apn;piv 


MiOO"J1MOOfflOCONiONNt"t"fOH(DO)lOOJHHClOONH<)'ffl 
OOOlOMWffiOffiWOOiOONHTfNSfflOOOEfflOlCCt^NOCNOO^N 
Oi-HOOOO^HOO^OOO^HOOOOr-iOOOOOOOOOOOOC 


•^8J— I9A8J 

A\ojaq     8pn;i;{Y 


•198J- 


•;89j— do;  0}  mdaa: 


,1,  »   I     I     I  jj 

Sg2  as© 


£ 

C3 

"¥7 


r-  O 
02 


>  co  io  o  -h  o  <n  oo  > 

IHOOONffiO. 


"  ::3tO(OHi 
-m  /:  i-o  cm  cm  co  < 

|  Tt<  co  ^t"s<  •<*!  t»i  < 


'HKJHOl! 
'  CO  CO  CO  O  l 


ocqNrtCSN 


lOcOOHUJiONO' 


1 1--  rfi  co  oo  cm  co  o  co  co  ■_:  s  <~ 

ii^oot^r^-HO'-ioooc'^: 

iOi01010)OOOOCCCC 


Pi  :phPh  :::::::::  :«# 


lOiOHiONOOOt^HCC-ri':.! 


OOOOOOCOOCOOOOOOC 


lOffl'fNmH 
6  6  d  d  6  6 , 


gj  §>£  M  M  M  M  M  M  X  ^  £  ^  £  £  g  -^  ^  X 

,?^e3c3c«c3c3c3c3c3cac3c3c3c3c3c3c3c3©«^arorc3c3c3c3c3c3-^'^ 

#  pi  M  M  W  W  M  W  K  M  W  W  W  M  W  W  W  H  W  Hs'H^^'ddddJddo&oQ 


be  M  DC  be  Ml 


^  ^  ^  ^  ,*  ,*  +*v 


£-5 

o  o 


lCMCO-^<i-lCMCOTfil050t>'000>0'-l'^CMCO'<*iUO«M>00 


CM  CO  -^  lO  CO  t«-  ( 


'—. 


?,: 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


191 


1 

i 

— 

a 

- 
= 
p 

C 

> 

- 
.J. 

5 

g 

1 

-z 

p 

c 
-/ 

p 

5 

? 

d 

= 

.3 

'3 
3? 

*d 
Pi 

93 

cj 

d 

-d 

| 

'5 

3< 

-d 

| 

.5 
'2 

1 

09 

'3 

o- 

■      «©a 

cy    mm 

©    ■ 

£    • 

oc     1 

o^  ; 

II 

mQr 

■"a 
j£ 

5  . 

-  r 
■r.   ~ 

-  rr 

z  * 
5-1 

't3 

■  a 

'S'g 

Si 

SI 

©   © 

mm 

g 

oo 

Is 

oo 

•OO 

Hflfi 

<N 

I? 

o 

l 

o 

JO 
OS 
33 

8 

8 

33 

© 

o 

O 

x  — < 

CNCN 

OO 

os 

-X 

s 

33 

•3 
os 

OS 

r 

a 

s 

3 

CO 

— 

E 
s 

3 

1 

g 

- 

— 

S3  3 

— <  C" 

O  O 

OtXDOO 
O  OS  OS  O1 

1 

occ 

—  ~-  £ 

oi  r.  r 

io  o~ 

OSO- 

1 

1 

o 
c 

x 

i 

OONHCCC'-O- 

ioooooo^oooooPhoo  oooo  oooo-=ioooooooo     oooosoooo     oooooobo' 

HOCOfflCCOONKNHOOltO'Kt-ifCCOtCCOlr.N^I'MJOOONWm         NMXiOOOO' 
MHCNO«!CWNINMINNrtffl(N01COi-OCqNr-<(NCOCOSMN«ICNfC; 


OOCOC^X  OOHiflOONONNNOiflXHi 


'OiooOHOoonoinisioiflOfnoo      omhovoioo      ooiOhouccoocn 
oocoos'O'Oooc^.r-'toooooc  oo  w  to  to  co  os  os  o  os  o  o  x  oo  —  o  o.  ©  oo  os  or  cs      o  r~  u-  a-.  c>  to  to  ^>      oomo:oi»nnx 

OS  OS  OS  OS  OS  OSj  OS  OS  CS  CS  ji  O  O  Oi  O  C-  32  ,  1  _ .  5  3S  O  O  OS  OS  O  O  OS  ©  ©  OS  OS  ©   CS*010^C^*0   ©  ©  OS  OS  Cs  ©  OS  Cs  © 


d  d. 
c  c 
co  co 

d  d 
oooooooooo   o  o  o33  o 

dddddd'Cddd   'O'O'O  o  Cfl' 

::::::::::     :  :  :psps  : 


:  d 

(odd 

:p3  :  : 


00  •*  CO  CN     o     o 
lOI't^iO     CN)      ■<*! 


00  oo 
CO  -sf 
•O     iO 


"       -r  <M  cot 
•o  io  >-o  i 


•C      ISIOUJI 


-H  00  < 

t--  r^  < _  _ 

HO  iO  ".O  lO  iO  iO  LO  lO  iO  «3  u-J  O 


^  o  in  o  lo  lo  io    io 


»     i^     O     h     ifl     N     *« 


o  o  o£ 


d  d  d  d 
o<o<osd 

©  ©  ©  O 

mmm^ 


c    o    o    o    o    o  o 
^  ^  Z  ^  ^  ^^' 


rH  IN  CO  l-H  !-(  CN  ^1 

odddddo'd' 


o  o  o  o  o 


O   IP  CU  CU  tl)   C^  "<5  O;      ^^   c3  c3  c3  c3 

o  o  o  o  O.H.5.S.S.S.9.S.S  S 


d  d  d  d 

o  o  o  o  o  o  o 

en  c/1  (/:  CO  co  coco~--.-- 

d  d  d  d  d  d  flflTfcca 

A  J3  fl  ^  ^  ,d,3  '     ' 

o  o  o  o  o  o  o 


.    ,doo« 


HiC*     CM 


o  c  o    o 
«Zi  j-Ts-T^;  a>  as  n>    o 

tM  So  So  trr£  IS  u.  t5 


^       r^       ^       ^ 


OOOP5 


M  «  R  H 

'd  "c  'O  ^ 

O  ©  ©  tt> 

^  PS  PJ  pS 


ill 

«  pIpI 

'd  *d  'O 
©  ©  © 
PS   P4PS 


©  © 

=  •=; 

cs  a 

x  x  : 


X  X 


■~  ©  © 

-d-drd 

X  X  X 


-  — 

X  X 


.© ,-  © 
i:rdi^ 

X  X  X 


.-  .© 
=  =: 

ce  - 

^-= 

X  X 


clo^ 

S£       •    • ^ ffl  ©  £ & £ W 

td«d         OO     .(pCSC 
C3c5       •^•d^c3c3(3c3,d 

^3^  ^  A     °     ©  rd  ^3  ,d     ^ 

tea;     OCPSP-OiccccPS 


pp  ©  ©  © 

.idtdcd  O  O  C  O 

'd  c3  C3  CS  '^  '-J'S  'd 

PSxx&oOCC  C 


OOticN     CO     ""S"     u~.-     CO     t^     OOOsO-hcN? 


t  -  y:  — 


l(N<NCM(NCN<McNtM(NCO 


l  CM  CO  ■*  UO  CO  f~  00 


r-H  <N  -h  ON  — i  CM  : 


oiONocao- 


CN 


H     ^ 


192 


OIL  FIELDS  OF  CKAWFOKD  AND  LA  WHENCE  COUNTIES,   [bull.  no.  22 


•siaxreq— lonpcud  i^nrai 


OC  n  & 

1-H  i-H  OS 

u  s-T »-." 
©  ©  © 


"O  iO 

— .  to 
5s  Ss 


>»8 


"5  O 


©  cr 


3> 

OsJ> 


§£ 


>-fe    s«. 


-'  N 


OS     -F.  53 

^Z^jS 

CHOtB 


U 


lis 


f    3£ 


iSSS 


n     h     **' 


a    qo   o   oc 


op 


c"H'e3 
Z 


00 


fi     Q 


•J98J— qjd9p  IT3J0X 


•j99j— i^depno 


rt  X  O  tO  H 
O  OS  ©  ©  CO 
O  OS  CS  O  OS 


Cj 
0 


ran^p  8AoqB  9pti}i;qy 


N  N  uo  O  Os 
CO  <o<  iO  iO  >o 

ooo  oo 


its  10  r-  — . 

I-  T  co  cn 


I-      to  CO  co  oc 


%Q9Jr- I9A9I 

■B9S    Auqgq    aptvimv 


5^ 


p9}eji9U9d  ssau^oiqjj 


Hi-IL-N 


•^89j— doj  oj  q^dga 


O  Os  os  os  Os 


©  OO  — I 
CC  XX  OS 


•    r3 
Z 


,     .  cs 

:  :« 

i -Co 

:  :« 


C30S3 
H"©   C   O 


o  c 

</3    CO 

►.►Jl 

03  03,0,0 

ii;oo 
cgcgPhP- 


x  o  -o  '. 

M00»-«l 

•O  lO  lO  i 


3C 

sz 


-3  © 
^Z 
0Q 


c  o 
ZZ 


PhPh 

do 


ooo 
ZZZ 

ooo 

OOO 


«!•«-«! 


6      ©  o 
|     ZZ 

I  Is 


o  o 
ZZ 


=3     CS  c3 

Sac 


Z  Z 


s     © 


co     0     W   Pi  03     O 


.©.©.2.2.2     -d     -2-2      -a  -ct! 

.Cd^,©-©       ©      ,0,©         ©     ©© 
OOOOO      tf      OOSSK 


,©    ^ 

o  o 


tl^ol* 


-r  CO        rp 


-i        Z 
1       * 

a  eh 


.2     t? 

,©       3 

o-  a 


£ 

s 

JW 

Z^co 

H     H 

W 

£ 

02 

QQ 

^Z 

ori  |Z 

IZ 

z 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


193 


8  : 

itg  :  :^  : 

^> 

IH 

:  .  a  .  .  Fj  . 

03 

C3 

ea 

a 

c 

i!IJi!i 

I 

:| 

tx-d 

is 

E5 

OJr-t 

!!f 

3  :S  : 

OS      ,             i 

-gj-s  : 

o 
© 

:8 

1 

ca 

DQ 

T 

°  :tf 

»sf 

p 

fcT 

03 

!  *> 

& 

- 

0 

«2 

1 

•1 

Oj   tC 

C3  C3 

1*1 

"3 

"ScNgi 
jhojO- 

g 

"o3 
J* 

!^3 

"a 

Ft 

c 

c^ 

o 

OS 

lO  <B  00  « 
>-H    ffi  CO.QJ 

or  7 

leg 

c 

F 

■3 -a 

£ 

ssas 

p, 

£ 

1 

^ 

SI 

en  CO 

C3C>  c3  c= 

:§ 

mm 

V 

"    ce 

0 

tnOC 

oc 

DO 

.cc 

c 

O 

0 

o 

ec 

:o 

tlfr? 

r 

c3  §  Fj> 

CZ    7t            Tt    -.^ 

h 

3p£ 

£ 

ooo 
•^1 

omo 

I- 

:R 

o 

mqCs 

h 

OOJ2 

oo    oo 

P 

o^c 

cl 

3 

cc 

m 

m 

10  *n 

O  O 

Ol 

% 

• 

05        • 

§ 

a 

c 

/- 

CN  CO 
O5  00 

O 

05 

A 

o> 

00 

c-. 

o 

S^ 

;s 

~1 

— . 

cn  co.-h 

£S3SS££ 

t-~  OC 

CM  t> 

10  01035H 

i> 

8S= 

toooooi'*  Nciwif 

O^OO^Ht-iOOO 

c 

COOOC5  o  c 

05  — 

— 

OOOr-l  C 

i-HC 

o 

^HO^-IO 

^^^ 

^^^^           ^r- 

rtT- 

HrHrtH^ 

~H^ 

_  _  ,H  ^  ^H  ^  ^H  ^  rt 

~ 

^^ 

HHHH 

oo  r^  o- 

CONOOiO!ON 
00  CO  «o  >o  to  <N  -t 

SS 

rf  r^ 

Si 

o  cr 

OOiVMCC 

COOlHOtOOOt^tiO 

r^i> 

Tf 

tji  ^<  -*  -^  in  -&  -# 

Tt 

T}<   Tfl   Tj<   CO  ^ 

CO  >* 

Vj'    L'j     Nj'     "V^    UO    I.V     "^     ^    "^ 

CO  CO  CO  Tfi  co  ■* 

o 

EC 

s 

E9>9 

lO  o 

o 

SC 

^S 

!D  ■*  l>  t-  C 

or 

(M  LC 

IC 

oco 

<Nr-( 

r- 

ro  co 

10  o >o 

SC 

O00HU5OHIM 

— 

otoooH 

U3  0HO!OU5U50HO 

X 

iO  O)  (N  »-l  CO  (N  Tf 

SoS§ 

O)  lO  "91  (M 
00  00  00  OS 

ffl»0)»00)(T 

oio- 

O0C 

a- 

00  OS  Oi  O0  CT 

00  c 

O30O00O0O0O0O5O5O3 

os 

e« 

CO 

CN 

<N 

CN 

o- 

!co 

CN 

SS 

(M 

CM  r-l  (N  rH        ;  1-H  CO  CO  CO 

-r 

i-l  IM  ^-1  CO 

£  S  ' 

a 

C  fl 

P 

a 

B 

:  a  s 

P 

fl  p 

flrtca   :  pj  pi  pj  pj 

PI 

fl  pj  C  PJ  P3  P) 

o 

o  o 

" 

o 

c 

■  o  o 

r 

o  c 

oooo    ,oooo 

5 

O  C 

o  o  o  c 

ssss>>ssss 

a  a  c 

> 

,  .a>>a.s 

a 

p 

\S  S  >-S 

P)  P! 

s 

a  g  g  g  g  g 

,0,0 -C 

<R 

,D  c3.Q,0 

|c 

la 

x 

.^^3   C3,C 

X2X: 

^X2X2X2  03X2X3XJX2 

p 

.Q^XiXJXirQ 

o  H  o  o 

c 

o 

c 

•  O  O  H  c 

o  c 

oooohoooo 

o 

o  c 

o  o  o  c 

M 

si 

« 

X 

Ph 

'X 

w 

PI 

- 

« 

tf 

:m 

£ 

-/ 

cs 

rt 

s: 

Pi 

tftftf 

a, 

X 

« 

M 

w 

« 

tftftftftfPn 

io»o  Tf    m      ^ 


>e    io      co 


2  *? 

jT  O 

it  i- 

"S  fa 


■  6 

.       ^ 
o    o    ^ 


d  6 

S  S 


6  2 


s  g 

fa      fa 


P    Qtf      P5PJ  ^    S 


»-H  CN 

6  6 

J  55  fc 

2  a  c 

3  S  (3 
fa    >  > 


55  55  » 
G  S  S 


55- 

o  <» 


CN 

6  6    6  "* 

^i^  Jz;  6 

CD   ®       CB  rj 

WW  M  fa 


ftft^ 
is  ^^ 

3  p;  © 


r-l  CN         -H      CN 


.2   8    .2 

^     g      X5 
OOO 


I  p1 


CNCO  rt     CN        t-h     CN 


0  «  pq 

•h  -O  73 

XI  CD  C» 

O  fa1  P3 


ooo 

oo  o 


r-l      CN      CO  i-H 


1*     I 

8  3 


■13  G 


fa 


194 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siajjBq— pnpojd  iBijraj. 


•199J— indfcp  mojj 


•;aaj— qjdap  no 


•}88J— 9WB\d 

mn^p  8AoqB  apnjiuy 


•aaaj— I8A81 
B8S    Avopq    apnimv 


paiBijgnad  ssaujpiqj, 


•;88j— do;  o;  iijdaa 


3  S  *  ?  £' 
ot«2  ©  >.2. 


OOO 


!  "5  ©  00  O  •**"  iO 
'  OS  *—  CTl  as  OS  06 


iTgeSosocjoseSoScaeJ 


iCO<Nt^.C500^r-IIM 


lOO^OXeaOONOOOONNOHQOMN 
CO^^CO^COCOCV3MCOM^OOCO'<l<TPiOC'5-<*,'<»< 


t^      '(NNrtiOOJ 

in  cm oo  -»  io  tp  io    -o 

ICOHTIIHNi 

pi  r)  e) 
o  o  o 

r/5  cq  cq 


H  o 
ootf 


.g 

o  o  o 


«  a  a 
8*8 -8 

o  o  o 


Nr-H        ,«HVHCC 

a  a   ;  pi  a  p  p  p 
o  o      o  o  o  o  o 

o)  w        to  in  w  w  co 

_9.9  '.9.9.9.9.9 
o  o  c3'",q3  ©33333  o 
•dfl*-  o  ot)  o  o  o  o  o"P 

:  \m&&  :«p5tfp5p3  : 


•*        iCiOO 


o     ooooooo 


(M  CO  OS  <N  OS  TJi 

T  iO  H  N  N  N 


lO         QOOOSOCOb-fO 
OS       OS  OS  OS  00  OS  OS  as 


.9 

[q  O  O  Op 

ofl'O'd  o' 

P5  :  :  :« 


S3    8 


"3    © 


fc  £ 


o    o  o 


-H        <N      O 

6     6  ^ 


o    o  o  o 


£   £ 


p        P        P  P,      P<Pl 

Ph     P-l     Ph        Tfl     WZfl 


U  .9 
p. 


333 

o  o  o 

tiaa 


5  o     , 

J^j2J  mco    i-h    (Mr- 

..  ,     ooo    6    6  6 

AA   £££  £  ££ 

o  o 

.9.9 

cp  4) 

PhPh      OOO   O   OO 


MMM    M    MM 


Eh    Eh 
t3  "d 


c3     c3 

o  o 


ooo      o      o 


ooo    o    o  o 


p.  • 

03  O 


©& 

02 


cp     p     a> 
H    H    H 

03       03    03 
03       <p    0) 

1-5      ^H-3 

03 
03 

i-3 

8  3 
J  o 

a  ,p,p,p 
o  ooo 

,P,P 
OO 

,p,p,p    ,p    .P.P 
OOO   O   OO 

C     00     OS 

O       rHN 

:- 

Tf<        lO 

CO     t-  00  OS 

<MCM 

HNM     t}i     lOCO 

I  M 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


195 


CD  CO  CD  ,2 

I  a  I?2 

ccZtaO 


2 


T3  CD^ 

fl.2  a 


£o£ 


ill 
'IS 

<   CS'O 

=3  tr 


03  O  O 


rH«D    "IOCO 


5     OO 


OiOi    ^ 

o3  eJ"J3 

OOtH 


'O'O  05*0 

00(80 

o  o  t>  o 

o  o-s  o 


Q.Q.P 


OCCNCN 


Q  bjOtuoO 

33 


828 


s-.   S- 
PP 


§82! 


oo-^oocor^cot^io      r-cocNcooocooooocNcoco      os»o      coco 
to  oo  c:  »  oo  oo  fh  n      ociHwioNcoNooNio      o<o      r^os 

OiOOOOOOO       OOO'-HOOO'-IO^HO        --HO        i-iO 


NNVNlOOSt^  CO  CO  TJi  th  G>  t-~  00  CO 
CO  CO  00  <M  t^.  tj<  lO  MMlOOOONNlO 
OOOOOOO       OOOOOSOOO 


cNcocNr^cor^coio 

CO  *H  CO  ^H  ^H  ^H  00  CN 

lO  ^  "^  ^  ^f  ^  *^  ^    ^  ^  Tj*  CO  *3*  "^  ^  CO  ^I1  CO  ' 


:S 


OMOi^O^OO   00  ■*  00  • 
Ci  00  C^  00  00  00  O  00 


tOiOOiONNM 


0000         00O) 


C^>  O  O  O^  OS  O  Oi 


CN  CO  CN 

o  o  o 


PhPhPh 


9  9  9 
3  2  2  2  o 

O  O  O  O'O 

p5p2PhP5  : 


COCN 

o  o 
5  2  2 


COCN  CO 

o  o  o 

223 

o  o  o 


ICNCN 

l  £  a 
)  o  o 


35 « 


22  03,0  C3X2       22 

o  o  J3  o£  o      o  o 

tftfcGPncotf     P5P5 


9.9.9.S  '.9.9 
3333  523 

o  o  o  o    •  o  o 


CO  CO  CN  Tfi  ■<*<  CO  CO 

oooooooo 

.911.9.9119 
',33333222 

oooooooo 


cnoo    t»    r-t^    r- 

l  CO  "O     lO     iO  »<5     iO 


iO     iCU)     i!5 


i-H     00  00     lO     O  CN  iO  < 
CO     OCN     CN     O00OI 


iiOcONiOi 
>  CO  COCO  00  1 


TJ<  rtNiO     CO     COi-l  CN 

6  odd    6    66  6 

&  £££  fc ££  £ 

,g  £  fl  £       -ff     £  £  2f 

a  a  a  a  a  'II  a 

co  cococo     co     coco  co 

,3  ,q,a,c|  A  &A  A 

W)  be  60  <afi    60    bCbO  bh 


—1 

CN 

*    io*    e 

o 

O 

o    o  o    o 

£ 

£ 

£  ££  55 

fl 

.d 

,d    .3,0    ^ 

a 

a 

a  aa  a 

CO        CO    CO        CO 

■3 

11 

fl       ,3,3       XI 

00 

fcfi 

M    MM    M 

a 

a 

M    MM    W 

CO  .-( 


^      UJFJ      i-H       T  CN    Q  T 

j  do    6    ooizjo1-1 

3'         -     ^        ^        ^     «CD      JZ 


W)     O  O      O      O  O^J  ^  3 


Tjit-CO     iO     CNCO      . 
rtCNCO 

o  o  o    o    o  o    .    .    . 

aaa  a  aa^^r^ 


*3 

as 

1 1 

MI'S 

W5 


.2  .2.2.2  .2  .2-rt  rr; 

i3  222  2  2  ®  eg 

o  ooo  o  otf  tf     a 

r»  oo  o>  o  t-i  cn  co  ■*        ic 


C3C8  o  O        Oc8o3o3 

«    PQ       .g       .g     .g   MPQ    ffl 

O  O      CD   <S      © 


o  o 

22 
oo 


.2.2-0.2.2    .2.2.2  .2  .2.2 

2  2  a?  2  3    2  2  2  2  2  2  ©  ©  ®  » 

OOPhOO     OOO   O   OOPntftftf^ 


111!-8 

03  03  03  03   u 

WPQ.WPQ  8 

fli   rt"i   /n   m  *•" • 


CN  ^ 


lOCOr-ICN> 


CNCO'J'     iO     CDNXCSOHN 


196 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.'  [bull.  no.  22 


•sjaxreq — ^onpoad  ibi^iui 


•}99j— q^dap  \w\ojj 


•^99j— q^dap  no 


•}99j— gireid 
rnn^p  aAoq'B  gpniiuv 


B9S  Avcqgq     apn^ijiv 


•:>99J— 
p9^j;9n9d  ssgujpiqj, 


*199j — doj  o;  qid9(i 


so 

§    . 
•rt  o 

to 


:8    8 


S3 


a 


■ot 

£  .02 


TO       OO 


O  rl  i-H 


.3      .3       >»  >> 

O         O        ^^] 
tf       P5       TOTO 


(NINffl 


O  O  O 
£££ 

O  O  tj 
yi  K  03 

Q  O  S 


;o    « 


!TO 


^^ 


P5      O     Oto 


I  cd  ^to 

S3         CO 


ICS  ~H 


■l"" 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


197 


S 


■sjajaBq — lonpojd  i^nrai 


•^88j— q^dap  ibioj, 


•jaaj— itfdop  no 


ran;Bp  8Aoqx3  aprnpjv 


•B8S    A\0{8q    apnitny 


•188J— do;  o;  mdaa; 


ta^S  ®  ^.2.2 


§2 


££ 


cod^r  oc 
ooocacoc 


'OCOO 


oc  oc 

c3  c3 


■*  o  "O  h  tp  10  rt  o  h  10  ^r  h  v  h  to  s  s  n  c  i^  ?:  l-  Lt  cc  c  l-  l-  w  e  u;  f  o 

TPMOHrpOCXL-MOHOOt-OlOCKOKK^-jrCTTHL'lrtr-eillO 
lo  N  t  X  o  -p  x  -r  X  t  i:  x  i ~  y.  :t  r~  r-  ci  r.  M  c  t  -  c  C  ^  r  c  w*  lo  os 
CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  *CF  CO  CO  CO  ^cf  CO  CO  CO 


I  CM  CO  lO  00  CI  :-  '  -  C .  ■ -  CI  iO  00  CO  CO  ■ 
(NhWhhINhhhhIN        CM<N< 


■X>OHt» 


<J!NONW(ON«ca;-rOCHTXI-C^->HNC  /:  -_r  ./-  -  y  rri  OC  iO  00 
OTPrHOiNHiOrHiooNiONcc  -  r.  /  ':  /  ^!c:  ;  -i-ccmooithio 
ooooooooooooooocooooooooocoooor^t^t-ooi^ococ  yy  x  x  x  x  oo  t^-  oo  oc 


|(MrH(Nr-lrHlNlHNrH        ,  (N  i-H  <N  . 


_i^cN.-ieoi-i.-<cMco.-ii-i.-ieor-it-itM 


oooooooooo  .ococcocccococccccoooo 


oooooooooo^cccccccoocccccocccooo 


C©  CO  CO      IO         IO      IO 


iO       CO  CO     CO     iO 


f~        IO     i-i     CO        <N 


<M  IO      t^      Tfi      ,_, 


o    o 


-H      OlOCN 

6    odd 


£   fc 


o  o 


fc   £ 


O      O      o 

£  55  £ 


Pi    Ph    Ph 


co  o  a)  a> 

ftftPn  ft 

o  o  o  o 

PhPhPh  Ph 


«;     <3  <j  <j     <; 


<;  <j<-<  ■< 


>>>>  >>  >>  >; 

fl)«      »  0)      0) 

co  w     w  i/:     3$ 

oo     «  »     fe 

WW  «  M  W 

ss  s  s  ■< 


■C  -C  T3 

o  o  o 

o  o  o 

t  t  h 

"S  "©  *© 

esj  si  N 


O     o  o  c     o 
O     o  c  c     o 

"3    "3  3  "o    "o 


o  o    o    o 


c3 

H 

c3 

c3 

c3 

w 

C3 
W 

waS 

ci 

S9 

c 

- 

o 

oo 

0 

.3    ^5 
O    O 

CI 

re 

•O 

CO 

t-» 

00  Oi  c 

CJ 

SO 

iO  CO 

00     OJ 

198 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sjaxreq— ^otipoad  reiitui 


•;99j— mdgp  pnoj, 


OO    GO 

03  CD 


!oo  o 


1m 


co  go 

WM    to" 
03  4)  03 


$3i 

f*  O)1 


03  Oi 


•}99j— qjdap  no 


•o  o 


00  O  O  >Q  CN  iO  O 
CO  00  00  00  00  00  00 


•}99j— atreid 
ran^p  8AoqB  apri^y 


NlO®fflN00CDNrtlOOC000 


X  t  -  «5  CN  t^-  lO  i 

1-H  O  I-H  1-H  rt  t-4  ■ 


cocot-~02>ooo*9<ooc 
cot>C2ior~coio>o'0 


•^99J— I9A9J 

■B9S    Avopq    apn^rv 


NNMHlON<CON 


CO  CO  CO  CO  CO  co  ^  co  ^  CO  ^J1  CO  ' 


i  CN  CO  t-  CN  •*  OO   CO  CM  O -^  CN  CO -*1  iO 
5  ■*  CO  CO  CO  CO  CO    CO  CO  »*<  CO  CO  CO  CO  CO 


•^99J— 

p9^BJi9n9d  ssgn^oxqj, 


'ssss 


*^99j— do;  o;  q;d9Q 


ooooc:."  f  /  -shoio 
^h>oc--.  moiMooNOioaioffl 
oooooooocooooooooooooooooo 


lOOiOHNl 

oo  o  oo  <N  r~  < 
r-  oo  i-  o>  i>  ( 


CNCNOOMMOOHCN 

OOCOiOOOCOt^OOOJOO 

t>-t^.ooi^-t^t^t^t^oo 


CN      ,  CN  CO  CN  CO  <-H  CO  CN 

I  a 

o 


.S.9.S.5  >*S 
3333  <&"~ 

O  O  O   O  >-. 

P^PSPhPhcv: 


R  0 

;  c 

oo    r 

a  g 
Sic 

c  c 

PSP3 


c  p 

II 


x:~ 

c  c 


o  o 

GO  00 

ci  g 

o  o 


fl  fl  a 
o  o  o 


<CN        ,-(      IcO^H 


■  eo 

rt  a  a   :  q  a 

.  o  o  o      o  o 

oo  go  go        go  go  oo        c/~  co 

>,a.s.s  >>a.s  .s  *JJ  ■  •  >>s.s 

03,0^X2  03,0.0  ,Q   d^^OO  03X2X2 

*-<000>-iOO  O'-'OO'U'O'-'O© 


_J*  O  O  O  _J3  O  O        orjoo 


O     lO     CNCN     CO 


CN     CO     r-t 


£     £     fc 
t£     >£     t^ 


£        £ 


S  2  2  2  2  2  rg 

Q}  ©  C)  ©  G>  CJ  X 

W  W  M  W  W  W  a 

«<*  w  w*  w  <i  <i  h; 


a  £    £ 


.  o  o    o 

*  1 55  5 

s  e  8  8  8 

O          O  (_     fcn          1-1 

S  5  fcp=i  P=I 


If 


5 

3 

3 

A 

3 

s 

3 

a 

3 

03 

03 

03 

as 

©   CP 

A 

3 

o 

c 

2 

o 

o 

o 

o 

o 

w 

W 

w 

CU 

tftf 

O 

o 

*x 

8 

<M 

Cl 

CN 

— 
CN 

CN 

CO 
CN 

CN 

s 

C^ 

O 

CO 

co 

i-HCN 

cc 

TK 

03  O 

as 

§ . 

53  o 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


199 


JO_ 

oo 


cd 
o  <o 


;      -30000^0000 

i^  a  ass  a  a 

oq     OO     OO 


u 

p 


a 


oz 


d" 


00  00  +3  +i 


c3  03  <g  a01 


d  e3 

OO 


CN  c£ 

OS  aa 


P  PI  as,® 

s/j  ^  •■"<  co  cm 

3  c3£  03  O  d  03  as 

OO  02  O  55  CO 


t-T  cd  t-T  cd  cd 
cd«~  »*=«£. 
"So  ^  io  oo 

^00    ^00  00' 

if  &2Z  co  w'' 
c3  *  c3  «  <g ' 

oqOccOO_ 

lOOJO 
COiO<N 


OS  ■— 
^H   <N 

o.  o. 


OS  00 


OO 

(NO 


00  OO        (OMIO 


^H__lOO 


rt<  CO        NOOONO 
t^  00         OS  ^H  CN  ■*  iO 

OO        O  tMOt-h  O 


MOiOHer'.oM' 


i  -h  O        OO  < 


CO  CO  O  CN  -h  00         tj<O300 

n  n  o  co  n  io       ioiok5 
NMhOOO      ooo 


CO  CO  CO  CO -*1  ■*         "*< 


a  2  gs 


'NOi-iiO 


»  os  rr>  — <  ir.  s  ■-  ■ 


■qn         -CM  CO  Tt<  CO  •<*< 


l  <N  CM  00  00  lO         OS 
I  CO  CN  rt         rt         i-H 


O  CO  iO  o  o 

CN  Tfl  T-H  T-l  i-H 


'COiO        CO' 


£8£ 


Tf  CO  CC  CO  i  ~  '  ~ 

■*ONaNo 


i  >o  O  o  o 


i  t^  00  00  00  ( 


ON         000010C0O00 

oo  io      r-  r--  io  o-  ~  ~ 

0000        cOcOOCOOOOOO 


C30  O  O  rj  O 

^o-d-qo-c 
cctf    5    !tf    ' 


.CNCO 

:  a  0 

.  o  o 

CO    CO 

'£  5 

222 
'd  o  o 


T-t    CO 

C  PI 

o  o 

CO    CO 

pi  g 

22 

o  o 

PHPH 


CM  CO      .CN      .^HCN 

c  p  :  p,  :  c  ci 

o  o    .  o    .  o  o 

CO    CO  CO        .    CO    CO 

a  a  j^fl   :  s  p 
22  os'2.222 

O  O  j-  CO  o  o 


CO  CN  -H  CO  CN  i— I  CO  CO  i-H  CO 

BflfiflflC 
o  o  o  c  o  c 

CO    CO    CO    CO    CO    CO 

S  5  5  £  B  5 

2  2  2  2  2  2 

o  o  o  o  o  o 
tf  £  p:  tf  pf  pi 


s  s 

:22 

o  o 


§§ 

CO'     X 


tftf 


§§ 

CO    CO 


tfp: 


;  cnco 

;  p.  p 

b-  b  ©  O 

>>    P    CO    CO 

ooas 
jSjSo  o-d-d 


ooo 
'd  *d  t3 


t~     i-H     O     <N 

CO        T»1        TH        TJ< 


co    co    co  io  io      loio    io    co  io      in  -&  >o 


o  o 

£55 


o  o 


CN        (N        <N<N        CNCN 


CN  CO 

H.    6  6  t2 

5  fc  55  * 

^    ^-  ^-  P 

r-T     CO  to  ±2 

§££g 

g  w  w  o3 

?  w  fe  J 


o  o 
o  o 


o  o 
o  o 

c  pTo 

a  c^ 

C3  C3^ 
^S    CD 


t-H     rr  00  t— 


55  5? 


•  o  o 


*   C3  CS 


ooo      ooo      o   ,X   CZ   Cz.   yZ    •    • 
Ztt     £££     jz;  ^  55  55  5500 


CNCO 

6  d 
55  55 


03     C3        yZ 

BW   55 


o  o 
55  55 


ooo 
55  5555 


■<£  p  cL  p.,  &j    pd 


^^^  ^i^:^  ^j    >    >    > 

COCOCO  COCOCO  CO     •— "     •—<■>— I 

03C303  03c303  C3dd3 

ftPEd  jJgjii  p  ^  ^  §  ?c'6    oo  d 


b»       fc.      •      •  •      •       03 

;WH     WW   pi) 


WW 
do* 


WbJD  W) 

www 


o    c 


£   £   £     pq  pcpcpq     pcpcpQ     pq 


BPC 


cd  a,  cd 
P.  Pi  ft 


ft  J  J  J  J  ftft 


03     cd     CD    ^3 

W    Ph    P3    O 

z 

O 

OO 

22  2   S3   fe   fe 

OOEH    f&    pn    fm 

cd     cd  cd  cd 
h3    Ph3P 

CD    CD    CD 

*     t>!     bJ     tai     b»'  ®  « 

S   CD     2     22 

h5h)   O    CO 

,0,15,0! 

ceo 

IO     CO     N      00 

OS 

5_ 

^H  CN 

CO  i-H  CN     CO     tj<     IO 

CO     t^rt  CN 

COTf  IC 

CO     t-     00     OS     C  ^h  <N 

CO  -<cf      IO      (CN 

OCOO 

200 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


•stajjreq— pnpcud  iBprai 


•%dd}— mdap  p^oj, 


•;aoj— mdap  uo 


PI 
O 
O 

! 

a. 
•<s> 

60 

o 


-18aj — aire  id 
mn^p  aAoqB  apnmpy 


•laaj — pA9j 
Avojaq     apnjpiv 


pa^j^auad  ssau^oiqx 


•jaaj— do;  o;  qidaa 


s . 

23  o 

2* 

02 


CD  CD   CD   CD   CD   CD 

NONOMM 
CO  CO  'O  CD  00  CM 
00  00  00  00  L-  00 

asaaas 

oooooo 


■OOB5KJO 


00  ooooo 

CO  CO  l^  00  CO 


co  co 


LOO' 

^8' 


oooo 
•oooo 


o»oooo 

LO  CM  LO  tO  lO 
r-HrH  CNCNCN 


I  <M  CM  CO  00  lO  "O  CO  CO  O  CO  CM  O  t>  CO  35  O  -f  Ifl  lO  I 


O  CO      -00  HwO  CM  CO  - 


(Mt-h      ■        t~CMCMCMCOCM^HCM<M<M<M<MCOi 


N  (D  LO  H  «  Ul  N  < 


■ij  l^»  U^  ^_J  n  F*J  <JU  Q_^  C_P  <~-l   'JJ  ■-'■    .'J    —     '  ~-    J-    —    —     J.    >    .     _-    _-     -  *   '    .     -*,    • — -   '-i^    T1   '.'J    ^T1 

co  io  lo  co  oc  cm  -r  co  ^h  o  "x  soac  »  ~  ccoonsooncomwnnm 
oo  oo  oo  oo  i-  oo  oo  oo  oo  co  i-  i-  'X'  i  -  x  x  x  x  x  x  x  x  i  -  x i  ac  oo  oo  as  oo  oo  oo  oo 


:  fl    :  S  S 


:  a 


:  s 

"d  o 


;  <M  r-1      INMH 

:  d  d   :  d  d  d 
o  o      o  o  o 

co  tn  to 
fl  fl  d 


H >-H        ,MMM        ,        ,        ,MM        ,MMM        ,        .        , 

SoooooooS  o'223  °  °  °22  °  'p-i'.o  |q  o  o  o 
o'd'd'O'd'dTi'a  o'cJ  o  o  o^t^ts  0  co  o  o  o'O'CJ'o' 

23  ::::::  :#  :###  :  :  :##  :phPSPh  :  :  : 


CM  O  —i  00  ' 


s  s 


(OMO      N      H         i-H 


P.  8; 


o  o 


CO  !>•  00     lO     CO  CM  i-l  -* 


■  tt  CM  CO     t-     >0 

odd    d    d 


CO"J<      t^      00 


O  J)  O  O  O      O  O  O  O  O  CD  CD  CD      CD      03 

OO  ^"^^"^OOO     o     c 

*->  *~>  u  j-T  tT   t-T  C~  s-T  s-T  S-T1""5  l-s  ^   l~>    l-5  'cS   15 

fekaaa   S  aaaafe^fe   te;   te  "S   rd 

•    •oooo  oooo i2i2 

OOOOO   O  OOOOOOO   O   O  S   S 


•  o  o 


o    o 


o 
ft 

^^  ,d  ,d    ,d 

OT    CO        CO        CO  CO 

C3  ci      Cj      c3        03 


55  o  o  o 

«333 

SOQO 


d>      CD   CP   CD      CD 


o  o  o  o  o  o  o 


ooooo    o 

22323  a  2222222  2  2  S  SS2  2  2 

OOOOO   O   OOOOOOO   O    O   P3   PhP^Ph    tf    P3 


CD  CD  CD 


P3    PicH^H 


I  C3  CO  •*  iO     CO     t»  < 


iOhNM     ■* 


■O     CO        t^ 


TABLES    OF    WELL   DATA. 


201 


42  ^-J 

CO  O  g  iO  00 


00   O, 


ft£ 


oo 


O     OOPQOO 


C    Cj 

^Pi 


O  0)  w  q;  A)  o  © 
Q}  05  «*-h  Q  a}  a)  <d 

'-no  £>o»on  ■ " 
OiOi  gcooooo 


C3  c$  O  03  C3  ^ 


of  I 


tt)  CD  CD  3 

«£S42-§-o 

NNCOpQ 
00  00  00  ftg 

cn~  c/T  w  "S 

03  03  03  CD  O 

ooomlz; 


isii  s : 


i  o  o 

>CN  CM 


i~    X 

00  00 


OOCMO 
(NNHffl 
O5  00O5  00 


CO  O  00  o 
00  00  00  00 


OOiOiO 
00  CO  t^  TJ< 
00  00  00  00 


IO  IO  IC  CO 
MOOV 
O0  00  00  00 


nnOHNte 


Tt«  t—  t-  O  CM  t^  ( 


hO)OM(DOHMOlo 

,-1  O   .-H  O  "H   —<  — lOOC 


WCHOO 


OOOi-H 


^oor- 

NOH 
i-HOl-H 


CO  CO  CO  O  00  ' 


iNNioaroMioioooicoo) 


_  - J  co  c  .  - 
'coco^cocococococo- 


O5-*J<I-~CMr-l00Tf<00O>CO 
00OCii-HC00500(MC0^t> 
CO-*lCO-<tiCOCOCO'Cf<-*i-^ 


lOONNCONM 
i-H         .-H.-H  COW. 


>  ■-<  Oi  CO         i-H  CO 
iCNi-h  CN        iH<N 


■-H  CO  Tfi  CM  I 
--H<N  CO  CM. 


)  00  00  00  00  00  < 


lOON(NiO(N0CMTf  a> 
tfCOiON  X  i  -  CO    JO   ~    ~ 

oooooooor^oooooooooo 


t^  iO  O  CO 


1 

c 

c 

B 

p 

c 

rH  CM— <        .CMrH 


:« 


9.S 
•2-°-^ 


9 
2 ,2 '3 

CO  o 


■9« 

r>  O 

P3  : 


(NHIN 

a  s  s 

OOO 

t/)    t/3    C/) 

s  a  3 


irtpipi   :^pi 


h  o 

-7  Pi 


fa   O 

coPC 


.— <        .CM        .CO 

ii  'M  :§ 

>£  :1  :| 

03",O  OXJO^ 
fcn  o'd  CO  O 

coPh  :«  :pc3 


g  : 

k   : 


Jo 

pi   : 


rHCM 

a  s 

o  o 

en  <r. 

3  3 


pntf  :«« 


H(Nrt 

OOO 


pciphph 


"■ 

c> 

CO  TJi 

0      c 

c 

0  0 

fc   ^ 

fz 

22 

|^      ^      j£    t^ls^ 

l« 

CC 

«> 

oc 

« 

rHCM-f 

03       « 

O      c: 

03  03 

rH  t^  CM  CO  OC 

>r 

c- 

L- 

c^ 

C-4 

c 

c 

c 

c 

c 

6  o*  d 

t 

t 

£■ 

CJ    O 

6  6  0  0  c 

c 

c 

c 

c 

c 

O 

!Z 

£ 

£ 

lz 

£ 

££;z;<ncv 

>-" 

^HCNCJ       . 

> 

> 

S     SS<M^^i^^^^ 

^ 

y 

V 

lz 

lz 

A 

CO 

0C 

CO  CM  H  j_ 

«- 

s- 

u 

k 

-   tTtTtTo  c 

c 

OOOOtyh, 

' &&&& §  i 

n  0  n  S  k>  v 

03  03  03  03  g  £ 

« 

« 

^ 

"<3°<j   6   6  j-T  rf  rf  rf  j- 

X 

r 

r 

r 

rf 

a 

c 

a 

C 

ue,  No 
ue,  No 
ue,  No 
.  Parke 

0 

p. 

P- 

p- 

0! 

Pi 

.  Parke 
.  Parke 
.  Parke 
amb,  IS 

E 

Ph       ft       p.,    ftfiZZ  ftftftftC 

2     2     2  2£^-ooooo 
5    6    5  £6^,Sflfl  33  c 

03         03         03      O3o303o303o3o3o3o: 

c 

p 

k   P 

c 

1 

cc 

-    P 
c 

ii    P 

c 

N  3 

0 

-a 

a 

P 

P 

PPP> 

> 

> 

> 

> 

>>>h^ 

hJ 

A  i_^  J  h4  cc  &c 

K- 

^ 

H 

_3  J  pq  cc  p:  pi  pi  pi  pc 

P3 

pd 

p: 

p: 

PC 

Ph 

-J-J+j' 

r 

t 

E 

£22 

■    '    ■ 

r- 

HHH 

333 

<9 

c 

<%■%<% 

655 

^ 

- 

rdro,,o 

<-<-<- 

c 

09 

- 

Pu 

c 

OOO 
C3  03  03 

^  ^  S    c 

I 

C 

c 

0 

c 

0 

c 

0 

c 
c 

b 

1    bi 

S 
a 

.2 
1 

c 

K 

O   »   CB'S 

—    •—    —  r^5 

c 

s 

c 
IS 

C 

c 

c 

IS 

C 

"-S 

c 

3 

c 

IS 

c 

IS 

c 

IS 

c 

3 

amuels 
imuels 
amuels 
eeper  ] 
eerier  I 

4 

1 

cc 
\ 

•a 

en  OT  O 
03  03-^ 
CU   CD  rM 

c 

IS 

c 

2 

c 

IS 

c 

12 

c 
IE 

c 
IS 

c 

IS 

c 

IS 

c 

IS 

Jj 

fa 

* 

H 

< 

HHHO 

0 

C 

0 

o 

ooooc 

0 

O  co  co  a5  J  h? 

P- 

& 

P- 

ftftOOOOOOO 

0 

0 

c 

Ph 

Ph 

Ph 

cs 

co 

T>  iO  CO  t~- 

(X 

cr 

c 

CM 

£ 

CM  CO  T  iO  CO 
CM  CM  CM  CM  CM 

CN 

OOCJsO^irt  CM 
CM  CM  CO  CO 

co 

iC 

cot^oooii-iCMeo'^'io 

CO 

t^ 

00 

Oi 

0 

1-1 

202 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siazreq — ^onpoad  rBi^rai 


•;88j— qidap  p^ox 


•;aaj— mdap  no 


ranpsp  aAoqB  aprimpy 


"\9Q} — \QA9\ 


•^89j— do;  o%  mfoa 


93 

ca 

£ 

' 

X       ' 

o 

+-^ 

+3    &        '. 

-     I 

o     . 
©    , 

- 

X 

<So 

«Oo 

- 
8 

>C 

o    ■ 

o 

n 

h 

1 

.(jOSrH 

O    l-    '— 

-r 

2^ 

o 

OS 

r. 

c 

<M   ©C«t»"S 

c 

.  o 

OX3 

e8 

o 

Is 

3 

c 

<Soo 

Is 

z 

X 

bd 

fc 

CO 

O 

Ococo 

SE 

C 

K5 

coo 

h 

>> 

© 

>>>.>>>> 

'- 

-       bl       S-       '- 

fiflfip 

o 

I- 

§11 

Ct 

OOO 

as 

Oi 

oo  oi 

•  CO  CO 

;OiOi 

da 

oo 

00 

o 

:gg 

c< 

Tf  CO  <N  >— 1 

t^c- 

o>      oo 

005  0)01 

•     oo 

rt 

:  :"*'- 

____    „_T-,^rHrtrt 

'-"-' 

-1 

:    r-"H 

Nonootorov^rHXNm 

OHtON 

:    ?SfQ 

■OCT 

•VCOlOPO'-IOllCrHCONiOtD 

■        •  TP   Tj 

■^•f-^TfiocoTfTfTfTf-^-^i 

iO       rf  -qi 

TJtlOifllO 

o 

•     •  to  r- 

OOMOlMHiOOONINHON 

<N      • 

<N 

<N 

MtowoeoioOHioo^ 

MNt<(NOOOMOSi-lOroM 

05050>o;oooa>ooc50!030) 

g£2i 

:    ££ 

ss 

•    -ooa 

OOOJOO 

0000 

-1 

.* 

HH 

tf 

Cs 

0? 

e< 

C 

1- 

re  - 

H  C 

1 

K 

op 

;    im'  ; 

a 

:  :  c  p 

fldrtrtrtPifld 

d 

:     a  a 

!    «  : 

o 

.    .  o  c 

oooooooo 

o 

.      o  o 

■      o 

•      .  S=j  C 

i 

~ 

:    32 

:    3  ■ 

,Q 

•      -^X 

o  3  3  3  3  2  io^laoBo 

■       ,0.0 

£  =3.2 

•    2© 

O 

.     .  O"  c 

"OOOOOOOO  CO  o'C 

•         O  O 

Tj  ^-rj 

ct 

« 

:  :«pc 

:##««£«£«   :pg  : 

:    tftf 

•  CO     . 

:    «  : 

iO  if 

H<N       Tf 

4  C 

OO      OO         O         CO      NCONNSb 

Tf  TJ 

Tf        Tf             Tf             Tf        Tf    Tf   Tf  Tf   Tf    Tj 

TP  Tf  Tf   -^1  TJ 

"    "*■* 

■rt  o 
CO 


OOO 

£££ 

'o'o'o 

'O'O'O 

fl  fl  PI 

P3p?p,   co       -cW   CO 


»0     ^-KN 

odd 


o  o 


■-CO  t^  i 


s 

a 

s 

s 

A 

A 

ft 

p< 

^ 

rfd 

^ 

fl 

tti 

CO 

QQ 

CO 

P=  ^  ts 
WWW 


o    ^ 

«     03  05OO  O^  03 

co  coco  |  |  |*-ico     C^CQ- 
cq   co  co  i-3  h3  J  co'  co'     Ofi 


aa 


Jz;  <n  co  I-! 

cf  d  d  d 
g^^^id 

S-lc  <u  <p  <u 

'|ooS| 

QoooW 


o  o 

©  © 

a  a 

o  o 


<NCOTf      ,-h 


o>       p<B<UOOOSO       oo       o  o  oo^       oo 

5     a  SSSSSsiS    iSiS    2222  3    32 

ft      ft    PufrtOOOaaQ     OO     OOOOiH     OO 


^    p4 


BL.ATCHLEY] 


TABLES    OF    WELL    DATA. 


203 


-o 

SI 
SI 


•d  © 
o"c8 


c3  C3  O 


xooiz;    og>o    a3 


©    ; 

+^ 

03 

CO 

"e3    : 

$1 

43      !  +i  +i  ^J 

©      .  ©  ©  © 

cn  »o  «o  co  <x>icio^H 

©a"" 

~  -c 

-O     „    «    . 

03  C3  O" 

elSgclcl 

oc 

O    coo 

la 


OOP 


Oi  Oi  Oi       05  OS  OS  os 


iO  <N  t-i  <N 


(NO        iO        00  »0  to 

CJ  Ci        OS        OS  OS  OS 


58 

oo 


QJ        ._       JQ        ._       _.        j- 

—  l~  -r  -r  X  O 
OOO  OC  OS 


r.OOOMO 


—  CN  X         NCONH-*10«0>00 
X  t~  -r       I-  t-  I-  X  i^-  C".  to  r~  •-  t~  t~ 

C  O  r-i   ooooooooooo 


—  cr  o 


o  co  r^  o  oo 

-H  oo  oc  co  co 

31  TP  Tf  CO  Ttl 


OlONHOH         H         CN  CT>  00 
O  CO  CN  CO  CO  CN         tji         rf(NM 

TPTjI-qiTjI-qi-qi  Tfl  Tjl-^1191 


lO*H1)l  CO  CO 

it-XffiOi       (NO 

I  OOOOOOOi         0505 


co  >o  l- 
C  C:  IN 
X  —  X 


iNNONXONOCNM 


CO         Tf  i— I  i 


H  CN  CO'  CM" 

cn  co 

'i  aaa 

fl  fl 

P 

5  O  O  O 

o  o 

0    W    Ifl    01 

,     q« 

.O.Q 
O  O 
tfP5 


g 

-do 


i-H  CO 


a  a 

s.  o  o 

!>    CO  CO 

3  O  Cd  «2  O 


tN 


O 


9  3 
c  o 


CN      I     Ii-hCN-h  <N 

cccc 
o  o  o  o 

CO    CO    CO    CO 

>>    .a   •   -.H.E.S.S 
cj    2  °  °S2 2 i2  o 

>-         O'd'O  C   C  C   C'd'd'd'd 

M    pi  :  :#£##  :  :  :  : 


tO       lO  to    «o 


CO  CO  CO  CO  CO  CO  to 


CN        (MCNCO 


O      I-H 

M'fc      6 


^      o  o  o  o 


•a-a  *s-±?+s-*s<a 

S  a  o  o  o  o.o 

02  02.0,0,0,0  U 


o  o  o 


66606066600 


000 


hhlH  t-iS-.t-.r-rJCCaC04'  O  CD   0)   © 

,2,2.2  ®Si!  o  o  o  o  o  oii  .H  .J3.H.S 

.,       — ■  — ■  — <  .-.  —  .-i  co  co  oa  to  09  co  rt  rt  rt  j     n  ri 

2  3  3     cemto  aiaiGQgggaggSg  g  g*£ 


mmm 


0 

000 

t>> 

0 

0.2 

0 

^j 

a 

fl^ 

2S2223  0 

.5  8 

fl 

XJ  fl* 

& 

^3 

£•& 

- 

0 

c 

0  oc 

cH 

O 

SO 

0 

OOOOCOP5 

M 

O 

§tf 

CO   CO   CO   CD   CD   CO 

cococo  cococoS?.2SS<^S 

SSS  ScBScxEiticltity: 

t-fc-t-  Uit-t-OOOOOO 

-d-d-c  -d-d-d  a  aa  aaa 

<S>  ©  o  0)<B<»^;^^fefefe6o 

flflp;  cccSSccc  o-S-2 

p,^^  pqpqpQpqpqpQpqpqpQoo 


o  2  2  2 
!3  i3i3i3 
O    OOO 


Nh        i-hCNCO 


lOCDNOCOO^ 


&s 

w'       H     £ 

^     w 

CQ 

od    1  ^  1  !z; 

CO         OS 

-i* 

0Q    l» 


204 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siaaj'Bq — :pnpojd  i^prai 


~cn   ~° 

«■*  k  c 
cSOs  o3C 
O       O 


Q)   ©   0)   0)0^)13 

00  o  CN  00  00  >c  _o 


is  r 


|CD 


C0CBCPCUCUCDCBCDJ8     .      '.  X  -^>  <1>  »  !K      •     ■« 

cpcp<»c»c»a>cBc»,2.J     \£a>SS£    .  tT 

HOOOMtOTfO'O'O   05  ^-?  00  "~  co  o  CN   ®  "tS 

—  ^C?2'S?!rl^?3J2      2  22  "?•  c?  ^  ^  42  ^ 


ooooooooo^ 


...    I  CN  CN  CO 

>OOOOOOOOC7s         O  Oi  to  en  O)  O1 
><35  o     „os     „    .    . 


03  03  03  03  CCJ  03 

ooooocooo 


o 


O     OOO     co 


hhNNinhhiNh 


p 


§gs 


o  cooo  >» 


OCNO 
0^*0 


•^aoj— m(fop  pnoj, 


•^9j— tudap  no 


laaj — eirejd 
uirvj'ep  aAoq'E  apr^i^y 


•188J— I8A8I 


pa^jjouad  ssaujiop^j, 


•^8j— do;  oi  mdaa: 


co«2  <»  >.2«2 


oFo 
S2 


O         »0         OOOONOONOCO 
CN  r-l  HNOHHHCOHCO 

OS        O        CJ01O1O5O5O5O1OOO 


>"  ~  cc  i~  y  tuoffl 
O  O  OlOO  O  O  OS  OS 


CN        iO  ~H  ic 


CO 

o 

eg 

o 

>OOINC[»H'XOll> 
lO  [^  N  (D  N  N  lO  ■*  N 

ooooooooo 

(N  f  ■«•  m  -r  O  iC  io  M 

ooooooooo 

s 

ooo  o 
ooo 

co 
o 

§ 

00 

oo 

OOCCOM«NHW 

f  M  CD  <D  (N  «  N  CO  CO 
NOlCtDiOC01,'*CO 

CO 

O  CO  CO 

■«*<  -*1   Tfl 

.      .oo      .....      . 

to     ......     .00 

■"' 

CN 

o 

OS 

3 

OS 

ocsooocasasoco 

HOO1M1000OC91 
O  O  O  O  O  O  O  O  OS 

CO 
OS 

co 
1  - 

00 

,»H      ■COCN 

:  rt  co'  a  a 

,  O-p  o  o 

co    5   CO    CO 

:.s  s.9.a 

_2.2-2-2J3-2.2_2-2  ^.0,0  °  °  °  °  ° 


.cotM 

:  c  s 

o  o 

co  co 


i-H        CM        CNCN  i 


00  OS 


I  OOO. 


O  t-n  CN  00  iO  , 


tNni" 


IOC-hCN 


o      o      ooooooooooooooooo  o2 
co     co     cococococccococot/jtrjcoco^^coco^^to 


X 


12 


2222222222222222222 

2232222222222222222 
ooooooooooooooooooo 

rtNM*iOcBNHNM^Ocet'«'aiOHN 
CN  CN  CN  CN  CN  CN  CN  .-<  rH  .-H 


2  2  2 
2  2  2 
ooo 


o 

"0 

:::::::  :tf2tftf  ::::::: 

*d 

CO 

CM 

.-HCNCNr^'t'COiOCO-f'ft^-^'COt^COCNCOCNOO 
N  l-  N  CO  1-  1^  CD  e  CO  CO  CO  CO  1^  N  N  l^  N  t^  CO 

o 

CM0OCN 
t~  I-  l~ 

CO 

I  - 

c 

2 

ooo 

222 

o 
2 

1 

CO 

111 

CO  coco 

1 

CO 

co     cQcocdcdcoco'co'co'cocococo22cQco*22HA         A     i-3>-3pq     PQ 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


205 


J 

- 

3 
I 

1 

i 

— 
a 

c 
- 
- 
- 

■> 

a 

.i 

— 
a 

>- 

9 
B 

C 

c 

c 

€ 

1 
0 

.  c3 

I'd 

;.d 

1 

111 

HJ'd-*- 
O'cc 

tf 

s 

00 

d 

3- 

— 

a 

■f. 

o3 
o 
o 

CD 

s 

LOO 

o«3«oooooooooo 

cNCOr-icocrrrocrco  — ■  o  o 
(N      co  co  co  co  co  co  co  co  co  co 

o 

O 

o 

s 

o 

a 

B 

O 

o 

o 

g 

600 
1,000 

600 
1,000 

IC 

99 

2 

OS 

(OffiOi 
OOO 

EN 

O 

00 -* 
S3 

=  53 

OO 

U5C*CNOOX 
O-HCO-H-HCOCO-H 
OOOOOOOO 

oo 

O 

X 

00 

oco 
a>oo 

X 

00 

O      ■  >— l        T 
O     "-I       o 

o 

00 

lC  O 

oooo 

3 

c 

1 

C 

1 

8 

c 

I- 

s 

1 

c_ 
c 

r. 
o_ 

x 
§ 

i  - 

o 

o 
c 

2 
c 

1- 

8 

O 

5 

e 

c 

1- 

o 
o 

c- 

c 
c 

en 

c 

■- 

5 

c 

re  i- 

1  -  "-T 

C  — 

t-  S3 

C  C 

s 

EC 

c 

NMOCHf 

-H   L.O  O  f  t-  C 

OO-hOO-h 

CN«N 

tCNNO 

oooo 

co  ai  eg  eo  oo  oo 

t^  -r  x  o  =  r. 
OOO-h—iO 

NscoKreK^«H(N«c^recc.fflT(i»«ONoeor)onNio«c»'*c»eootiO"*a«DOi»Nw 

^^Tj<rt<Tf<^Tti^Tp^Tt<Tr^T»i^TtiMTt<Trc^coTr'co^^^eo^^^^^^^^^^^^co^TrTi<'^ 

N  IO  -h  C.  C.  O 
^3*  ^f  ^  CO  CO  ^J1 

■X       "ti-iffiaNOMNNNOiNOi       'W<*       .       .00       'TTCi.-  «0C  l^  MCi  N       .  1-- 
.  Tf  ■<»<  CO  CN  iO  CO  CO  t~-  lO  CO  ■*•  ■*  t>-      •  •* 'SP      ■      -CO      •  ■*  iC  H  rt  CO  M  TfTf  co  N      • 

■  CC  va  CN       'CS-PTN 

•  eo  co  co    ;  <n  cn  co  io 

MN-<0)0(0 

KooTi.ioooofCCicxewHOoeoMNr'MSNNicoeKHOO'v 
oi  a  o  o  cc  ?.  x  z  c.  c  »  o  ©  a  o  oo  x  c.  cc  o  x  c;  «  c.  x  »  cc  x  o  «  *  «  oc  «  o> 

00~rOcOOO»-0  00 
OiOO00  5<©00  0)O 

oooooooooooooco 

t^  w  Tf  X  -r  N 
00  O  00  00  00  00 

COCNCOCN 


d  d 
c  c 

73    73 


-HO 


2J25 


d  g 

c  o 

73  73 

a  & 


I  o  c 


.  :  :  fl 

ooo2 
•ceo  o 

:  :  :p3 


ii  : 

.    73       ' 

£pj  : 


!> 


— I  CN  CO  <N  -h  CN  !  — I  CN 

cccccc  ;  d  d 

oooooo  oo 

737373737373  .7373 

.S.S.S.S.S.S  ■  c  ~ 


n 

0 
DC 
P 

c 
I 

73       ,    73 

.S  >-..S   •   •  >^.t  id   •   ■   - 

2  cs  3  o  o  ^3  2  c  c  c  2  2  2  2  2  2  o  2  2  o  o  o 

o^o'O'Oi-oo'C'O'Cooooco'Ooo'C'O'd     t) 

tf^tf  :  :£tfff  :  :  :tfpdtftfp;tf  :p;tf  :  :  :      ; 


—  £1 

o  c 


LO  Tf  N  N  N  C  O  ©  X  N 


■NCCifliO'Tfw 


CO  t^     lO 


|~  i~  '~     o     iO     >o     »o 


O     COhCMlO 


o  6, 


.-=.-=  &Z2Z 


Tf"«t^-HCOCNO3  0C' 

dodo  odd  do 


CN     CD  00     -i     0)t^M«3i 


o 

o 

o 

o 
2 

o  o 

o 

o  o  o  o  o 

o 

c 

o 

o 

o 

odd 

zzz 

6 

d  d  d  d 

B 

c 

1 

d' 
o 

d 
o 

03 

d  d 
c  q 

a 

0 
CO 

lllll 

d 

c 

| 

0 

d 
c 

ep 

= 

c 

c 

CD 

??i? 

03 

H  H  "tl  TI 
c3  c3  c3  c3 

&£££ 

O  OO  o  OOOOO  O  O  o  O  O  mmm       xn  mwuim 


c3  c3  C^  c3  ^ 


C3      C?  0?  C?  © 


c  c 

22 


"S  "H  V.  V.  V.  V,  ^  V, 

££££££ o£ 
&  $%%%%%% 

C3c3c3c3c3c373c3 

oooooooo 


C   0 


ic3c3c3c3c3c3c3v^ 

^  £  £  £  £  h  t?  £  £ 


C3c3c3  c3     C3c3c3c3 

OCDCD  CP       Q3CPCDCU 


OCvffi 

o  o  o 
OOO 


OOOOOOOO-S- 


o    o 


o    o 


oo.d.d.cj   ^-    ^   ,3   ^3   ^1 
£SCOC    OOOOO 


C3  C3 

o  «,  t, 


--c  i  -  y.  ~  ~ 


CO     t^     00  OS  O  — i  CN     CO     -*i     io     CO     t~-     oooo 


CD  G}  d3  O  CD 

Ph  PhP,P,0, 

O  OOOO 

o  OOOO 


CN     CN  CNCN  i 


206 


OIL  FIELDS  OP  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


siojjBq— icmpojd  p3i^iui 


•%9&i— t^dep  p^oj, 


•}89j— t^dap  no 


umjBp  GAoqe  apn^i^iv 


■}89J— I9A91 

■B8S  Avoiaq     apri^y 


•j98j — do}  o;  qjdaa 


5  S~  F3  9  « 
co<5  a>  >.2.£ 


ft  • 

c3  O 


23  o 
CO 


»-T   1  >h" 

(_; 

^  • 

cp 

C3      1  03 

m 

03     • 

*  :* 

* 

£     • 

o3  :  o3 

eg 

CO     .CO 

GQ 

CO     • 

*5    '+-T 

+S+3 

•     • 

t»    •  <u 

CD  CD 

CD  CD 

Tfi  <D  O  O  iO  O 

lO  ,5>  »C  ,05  t»i  CD 
oo  *-*  00  *"•  00  00 

_i-J      -O      „     „ 

fl 

~  _c 

3$3So8S 

x 

S3& 

o    a 

CO 

OO 

o      oo      oo 

2    gg    82 


CD  O  OiC  lOiO  CN 
«0  r~-  iC  CO  iC  CO  CO 
00    00    0000    0000    00 


2* 

O  v> 


oo  U>«<- 


g!3 

00  OS 


coco 

t—  00 

oooo 


CO 

s 

I 

22 

t—  00 

ooo 
i— i  o 

O00NOO 
HOiNcOX 
i-HOOOO 

■o 

TPpO>rtOiOlONt>.tDCOCO 
XNO^VOiONOrHXN 

Or^rtOr-lrHOrHOl-HOl-H 

I 

o 

■  O 

CO 

CNt^ 

coco 

coin 

COT* 

CO  TT  Ttc  tH  tji 

-T 

co 

®HrH050lOlOCOW*tCll< 

i-Hr^oiiocooiTtn-^ooooor^ 

Tt<  CO  CO  TF  CO  CO  Tfl  CO  Tfi  CO  J_  CO 

o 

QOHOOH 


CNT? 


S2S! 


HO  00  OiOOCOO«5iOMM<500  o 
100  lO  OiON^-tNCJiJiNiOOtO  o> 
100         00         Oi  00  00  Oi  00  00  Ci  00  00  00  -^  00     00 


a 

O  O         0,Q 

:  :      :ps 


«  :«  :  : 


i-H  CM  i-l  <N  CO  i-H  CM  CO 

o  ooooooc 

to  t/3  (/i  to  c/]  en  co  t/i 

3  SSSsSSS 

3  2  3  3  3  3  3  3 

o  ooooooo 

rt  pi pi  pi  p3  p5  pi  pi 


— l<Nl-H 

(3  fl  fl 
o  c  o 

w  »i  y 

S  S  9 
333 

c  o  c 

Pi  Pi  Pi 


i-l     CN 

.J  I 

4)    O      _Q 

oPi  Pi 


lO       »o       lOiO       *o  *o 


6  o 

3"o 
oo 


6o  cnJ  CO  •*  CO  »o 

££  oo'odd 

fef  ggggg 

O    O  CO    CO    CO    CO    CO 

r"ir~)  cococococo 

^^  03  03  03  03  03 

ss  £££££ 


0     fl 


d  d 


Cj   in 


CU   CD 

ftft 

o  o 


CD  CD  CD  CD  CD 

So  tuD  5Jo  Sjd  Si) 
o  o  o  o  o 

MWMWM 
el  a  a  fl  fl 


cppqpqcQpq 


11 

PP  P5 

CD       CD 

Pi  Pi 


CNCN         COCO         COCOCOCOCO 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


207 


1 

o 
as 

00 

a 

- 

•2 

— 1 

S 

CO 

a, 
CN 
oc 

c 

1 
1 

09 

"5 

o 

0«5 
O  CN 

CN 

CN  CN 

»U50 
CN  (NO 

1-H  .-ICO 

o 

2£ 

o 

02 

09 

DC 
09 

35 

35 
BO 
09 

00-4 
05  01 

CM 

OS 

OS 

O  CO 
iO  CO 
COOT 

o 

? 
OS 

c 

5 

00  o 

oo  as 

CN  lO 

Old 

oo  c 

■ 

MMC0M«5HO*^01*!0(0ON'J,NHHNrt00ONM>rttC00O0>HC0NNrtNNC)W«N!O'<rMHflCN<ir00  0> 
.-iOi-iO^Ort©^©©^©,-iOi-i©.-i©i-i©rHTH^Oi-i©©.-i©OOi-<i-i©©©i-iO©>-i©©©0©rtO©rH©© 


t^  t^  t^  t^  Lf5< 

00O00O01L       . 


ico^co^co^co^co^cococo^w^^coTFTr^coco^^^co^^co^rr^^^oo'VTj'eO'*''^ 


ONN?q(NcDwxiop:0'»'*<»Hi.'3NoiN«(art!o     •  cocNoor^o--©^coiooocNcoioa5ioio©co^HC©cNcooo-w'iaoo 

i-H  CO  -*  tj.  ,-,  tP  i-i  CN        lOiO        W        CO  r-i  (N  CO  tH  i-i  CN  >0  CO      •  CN  i-i  (N  CN  CN  CN  i-h  CO  CO  CO        hhhco  i-h        i-h        hNhhN 


CO  CO  CN  CN  00  CN  CO  ( 


'NoooiOHNin 


...I00NCOC      - 
t^Osr~09t>-c3>OOI^0»03t^09CO00^>01' 
000000  000000  0005  0000  000000  00  0000  00  < 


CN  >o  r-  CN  00  t.      - 

OOlOOStOlOTPOOCOOOCOCOt- 
000000000000000000000000 


J'lOCOcDOOCOmcOHONOOCRHNTj't^OiNNCON 
-f00COiOwcNcOiOCI>'<}'I^CRM'q"ONNe<IMN'<' 
0©000000©©©00©0>0000000>OSOiOOOOOJ0001Ci 


i-KN-hCNi-hCN^hCN^CN 


I  CN  -*  CN  .-H  (N  i-H  CN 


99  99 

o  o  o  o 

CO    CO  CO    CO 

fl  1=1  ci  a 


#££( 


o  o 

CO    CO 

5  9 
S3 
o  o 


S  9 

c  o 


o  c 

tig 


a  a  c 
o  o  o 

CO     X    CO 

3.5.5 
o  3  3  3 

T)  o  o  o 


C'CC 
o  o  o 

CO     CO    CO 

.5.5.5 
3  3  3 ' 

o  o  o 


o  c 


co  co  co 

5  5  5 
333° 

O  O  CO 


iCNCOCNi-i      .CNCO' 


iCN->r  i-iCN 


;  ci  ci 

>  o  o 

:  co  co 

1.5.5 

>  O  c 


.CO       .  TT  i-H  CN  CO  i-l  CN  CO 

iOOOO         OOCCOOOO      .  O      .OOOOOOO 
icocococo        cocococococococo     .co        co  co  co  co  co  co  co 

i555S  '5. 5  555. 5  55  >>5  >1 5  5  5  5  5  5 .3 
13333^33  3  3  3  3  3  3  <s'3  es'3  3  3  3  3  3  3 

>ococrdcococooct-o£oooooqo 


oo    iv    oo      r- 


cn    om 

00     l- t- 


,M     H     NV 


fc     £     £ 

cf    cT    cT 


fc  £  fc 

cT  cT  a 


fc  £ 


.5  .5 


d  .d  did 


c3        c3        ri        ct      73      c3 

s  s  a  a  a  a 


rf    .cf 


«       «    ^O!    CQ    CQCQ      O 
■o 


a  a  w  a  a  a   a  a  a«;  «i  «;<! 


9  5     9 

CQ    CQ       CQ 


<5  <J    <i    «<Q 


So 

d* 


gpq  pq  »eq  .g 


fl 

CI 

CI 

C3 

C3 

03 

Pi 

Pi 

Ph 

CQ 

CQ 

CQ 

5 

e 

o 

a 

o 

2  5 

P3 

CU   <D 

«P5 

c 

0 

0 

O 

C3 

C3 

£ 

t 

£ 

t- 

X 

09 

— 

05 

r^ 

— 

O 

co  t- 

X 

2g 

T5 

t  - 

R 

•N 

CN 

<N  CN 

CN 

IN 

CO 

CO 

208 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no. 


1 

o 
o 
O 


•spjiBq — ;onpojd  p3ni_i 


laaj— mdap  pnoj, 


•^aaj— mdop  no 


ran^p  aAoq'B  apnipiv 


B8S     AYOJ8q     8pn}T}\v 


•»99J— 

pa^Jiauad  ssau^opqj, 


•^88j— do;  o;  tndaa; 


3  o^  go  g  ffl 


03       03_5_> 


II 

o  o 

AA 

W  03 


_    _ 


CCCDNrtOONiOOO         OOOl-^-fC 


iNVlOmomOHlONQC^HNNl 
lOOHtaONNfflfflNOOfOOi 


Tf  H  C<5  »  IN  CO  1C  M  NHOCDONrOOiONOlOOCliOCONnOimcON 
fflO!CNM(Ot^W  l^NOtOOO-^'COOXSOiMOINNMMMfHiOrtCO 
CO  ^J1  ^  CO  "^  ^  CO  "^         ^tf1  CO  "^  ■'J1  CO  ""G1  ^  ^  CO  CO  CO  ^  "^  ^  Tt1  ^  *G*  ^J*  TT<  CO  ^t1  ^* 


CO  CO      -CO  CO  CM 


n  tihc  rt  •*  in  o  n      t^iooocN-rio 
coNcomoMves      w ■- 
oo  oo  oi  oo  as  — 


I  00  a>  00  CTs  C3  00  00       03 


lOOON-riCO^OONNNHOiOXWOIOtOI 

ooooa>ooo5a>oooooooocioooooo5ooocoooooo< 


.9.9.9 


o  o  o 

www 

S  2  S 
■~  2  2 

o  o  c 


.-HIM 

II 

a  a     i 


CM  CO  r-<  <N  CO  rH 

C  fl  fl  fl  fi  s 
o  o  o  o  o  o 

w  c/3  xn  m  in  m 

B  .9 .93.9 .9 


:  c  a  a 

o  o  o 

m  m  m 

a  a  c 


________  ________ 

tftfpitftfpjtfpj    tf  CH  ix;  tf  Pn  tf  tf  PH 


ooo323°  ooo2 

1  """*  O  O  O  *—  '—  T3  *_  o 

rtpirt  :  :  :  :p3£ 


,-H        ..— 1CM 

o  o 


o  q  q  q  q  o'C'd'O  o  o  o'd'O'O'd  o 


tftf 


CM        •«»<  Oi  -h     (N        CM     lO  CM  _>  CM  r-     CO     CO 

00         XNOO     N         1^     HINiO®*     t-     «5 


CO  CM  >— I      _>  "*i      1CJ1 

666    6  6    oonhn  ^h 

^ZZ  -^  ^iZ^666  6 

.9.9.9  .9  .9"  .9~.S~'zl'zi.'zi.  ^. 

"£ "C "£  "C  "£  ti  "£  ^  ^ -*-*  ^ 

03  03  C3      C3  -      S3  <S  £  „   _  £ 


o  o  o 


:^^  c3    c3 
„„PQ  pq     • 


i   O  O  O  O  0^2X2_j  _j  O 

AAA  A  A  AAggg  »  3 

OOP  O  O  OO^tf  Ph  O 

r-l  CM  CO  Tf  "O  ©NXOlO  FH  .CM 


&6 


33  © 
_^ 

03 


blatchley] 


TABLES   OF   WELL   DATA. 


209 


e 

<- 

0. 

— 
X 

J 

i 
a 

-5 

s 

C 

5 

r 

3 

a 

I 

c 

1 
i 

1 

co 

y. 

i 

lO 

8§    ;SS 

S 

?. 

JO 

g 

s 

3 

o 

<N 

s 

s 

8 

g 

£ 

U5NO 

os  os  os 

09 

OS 

a. 

t-      'MO 

OS     ;So> 

CO 

os 

ooos 

J0 

<NcO 

oo  oo 

CO 
0B 

CO 

36 

1 

2 
c 

5 

5 

3- 

CO 

in  co 

55  — 

1^ 

CO 

or 

ec 

eg 

CM 

C 

c 

c 

£ 

C 

C 

| 

c 

Ifl 

5 

c 

cn 

•V      CO  OS  CO  »0  CO  OS  CO  »0  CO  O  rH  CO  00  t"» 

oo    oo  io  cm  oo  ic  o  as  as  as  co  os  co  ci  i— 

O     OOOOOi—  OOOOOrH  Or* 

HNHOO 

a>oaioo 

TTCS0^0CC0COCN^00C0CMTpcN^0CCOCCCCeMCSGeCMCOrHC5rHOsCM00'<J'I>>     »-h     HVNH^OlOOOt^OtOHOCHt^flNN 
•«»<  ■*  •«»•  TT  ■««  T)<  Tf  TJi  ^  ■»■  -*t<  Tf<  •>Ji  tji  CO  -v  CO  •*  •«•  ^  CO  •*  co  •*  CO  ■"*■  CO  T  CO  "«<  CO     ^     ^  ■<*>  ■<*■  -v  T><  CO  t -<j<  •>*  -w  CO  **  co  »o  -»•  »o  ^r  -<t< 


^r      •U5NONN!Cu;o)!OCCO(0'*t»      ■hMOO'«,OhiohO'»ONO     CO     O      ■OOTfOOiOCHHtOtOOHtM 
rH      •  ^H  ■«<  CO  CO  CO  i-l  CM  CM  rj<  i-l  CM  t-(  t-H  rH       ii-H         HrtHHMHMHnH         T-l     CO     ■**       •  CM  CM  CO  CO  CO  T  ^f  CM  "*>  »«  CM  •-!  CM 


0("5-HOOO>«)(NONOOcNrH40vOM'irCOO(NO'»00)NNNNNO)<N     OS     WNM^M^iOMwiOHOrtinNNOCOli 

-noocooo>oO'*ooooso5<0'Hii-o)0>iONO(ooot>.o)NO)inrHM    co    oo  o  -f i^-  o  -^  io  to  cc  cm  oo  tt  os  co  as  -*r  os  oc  i 
os  os  as  as  os  oo  os  as  as  oo  as  as  oo  oo  oo  os  oo  oo  oo  os  oo  os  co  oo  oo  oo  oo  oo  oo  as  oo    oo    oo  os  os  oo  os  oo  oo  oo  oo  os  oo  oo  oo  oo  as  os  os  oo  i 


,00  CM  00 

las 

o  3  3  3 
x)  o  o  o 


sa 


-hCM 

8  8 

c  o 
co  cn 

a  a 


~3 
«   : 


O  Oj2, 

:  :pst 


i-Cd  o  o 


r^CM      .  CO  ^H  CM  i-H  CM  i-H  CS  rt  CM  ^H  CM  i-H  CM 

c  a  :acccacccccac  i 

oo  .oooooooooooo  o 

coco     .cocococococococococococo  co 

S.S  '  S.9  9.S.S.S.S.9.9.S.9.9  .9 

33  o3'3333332S333  3 

O  CO  oooooooooooo  o 


,  cp  cm  rH  cm  »h  r».  ep 

a  a  a  a  a  a  cj 
o  o  o  o  o  o  o 

co  co  co  co  co  co  co 

casSScc 


:«tfpHpH 


^„.9.g^ 
■§■§•§■§■§•§■§■§■§ 


CN 


t>.     CO        CO     CO 


S?2§£ 


«OCMC0OS     00 


o  o 


o    o 
55  55 


o    o 

55   55 


CO 

6 

d 

z 

^5S 

pq 

Birch 
No.  1. 
No.  1 
No.  1 
Birch 

-a 
p 

oHH 

H 

H§g§W 

K 

pq 

pq 

ha 

=<3 
< 

A.& 
Wass 
Wass 
Wass 
A.  & 

•8 
< 

•  •        ;       ^        •      •        •      •    •    •    '    •    '•    •    •      •       •      •  d 


00     CM  ^h  CC  ■*  iC  >-i  CM  00     CO 


fc     55     55     55     55     55     55 


o    o      o    oooooooo    o 
55  55     55  £55  55  £55  55  55  55  55 


o    o  o 
55  5555 


t>  <J  U  <->  <J  «  <J  k^  U       U  <JOOCJOUUCJ<J(-> 

E-tHEHHHEHtH       ?     BH     H   H  EH  EH  H  H  H  H  H   H 


^3  ^rd 
o  o  o 
EH   EHEH 


CH  C  d   3  3  Dr<  rH  Q 

o  o  o  o^ld^  o  o  o 

.2  .2  fcfc  b  fc:-<-<^  E  fc  E 

,c;    ^d  o  o  o  o  q.o.o.p  ~ 


*0  'O'O "O"  cu 'O 

C3  c3  C3  03  03  C3 

&  &*  ££££ 

'O  t3  "O1  "O1  'O  "O 

W  HWSWW 

«3«3     *.  oo«o<3<3=3 


O     O   OSS   S   SSSSS   SSSSSSSS        MPhPh 


s,  °  ° 
SfeSSeSSSS  3    3  33 

Ph  PmPhPhPhPmOOO  o     o  oo 


O        <-H  rH        CN     CO        "P     >C  CO  C^  CO  OS  O  i-H  cm     co        ■*•     «o  CO 

CO  CO  1— I  i-H  i-H      I— I  rH      rH  rH 


•f      ICCON      CO 


I  rH  CM  CO       "Cf 


I-. 


ICMCM  CM     CM        CM        CM 


-14  G 


210 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


•spjjBq — ;onpojd  p3ijrai 


■}88j— q^dep  xb%oj, 


•lea;— mdapiTQ 


pjoo 
U  aft 


0*53  £ 


ft 


S3  §8 
3  3 


CO 


* 


um^Bp  9AoqB  apn;i^y 


i-Hi-HOOi-HOOi-Hl-li 


iOi-iO»f-iO 


lOOr-H  Oi 


•198;— \9A9\ 

B8S    Atopq    opn;i;xy 


-rf  <N  a>  CN  rH  CO  ( 


1  CO  ^F  ^  CO  00  CO  ' 


pa^Bjjaned  ssatopiqj, 


tfiOOOCN 

rH  rH  i-H  CN  CN 


•^89j— do;  oi  qidaa 


iCT>00000C0000CT>00O500( 


lOlONCOOO-flOi 
00  00  OS  00  00  C5  00  ( 


iNiHNHMi 


^rt.n  a  g  g  g  g 
c3  5  3  2  3  3  3  2 ', 

t-OOOOOOO 


HHMHNnHMHMHn 

oooooooooooo 

(nintnoiMintoioi/nnoii/! 
flPlflPlPlflRPlflarta 


##«£####«£#« 


00      OC  CO  00      00 


,_,     QOrH^     «c 


ft    ft    ft    ft 


d 

d 

d 

6 

6 

fc 

££^ 

fe 

fc 

fc 

% 

fe 

©  aW 

,d 

■d 

^ 

r^ 

a 

"3 

33  a 

S 
no 

a 

QQ 

a 

xn 

a 

o 

O  O     . 

ft 

Qft<^ 

^ 

<! 

< 

< 

< 

03O 
S2 


2  O 
03 


03  03  e3  03  03  o3  03  OS'S  *g 

£  £  £  £  £  £  ££tf  |§ 

00  Oi  O  ^H  CN  CO  Tf>  lO  rH  <M 

r-l  rH  <N  CN  CN  CN  CM  CN 


o      o      o 

3    3    3 
o    o    o 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


211 


| 
1 

0 

c 
c 

z 

c 

c 

c 

c 

c 

i 
0 

g 

c 

1 

K 

1- 

1 

co 
3^ 

a 

a 
— 

CO 

y 

Pi 

c 

pp 

,- 

y 

R 

c 

c 

-r 

a 
a 

0 

1 

r 

5 

"3 

1 

CO 

c 

u 

o 

a 

j 

cc 

a 

i 

— 
p 

T 

7 

T3 

s 

yj 
c§ 

a 

I 

o 
"as 

i 

1 

• 

• 
; 

CO  -^ 

co-«< 

S 

8 

s 

-       (1 

ft  ft 

1Q 

1 
1 

s 

o 

lO 

t^ 

§ 

(N  CN 

00  (N 

05  0 

o 

85  : 

o     • 

<NO0 

NOW 
O  CO  00 
OS  OS  00 

CO00O5 
05  lO  1^ 
00O00 

co-^ 

CO  kO 
c3iO> 

CMOCN 

CN  OO  -H 
Oi  05  OJ 

t- 

Oi 

a 

coco 

O  >— I 

OONU5!ONO)0000)COC3)ONNrt'*lOOlONcOrtiOffllON         NQC         t^OlOKOOtONNMOXM 
^rfmcOfmM'rcOCOtO'roCtOOINOXrtOCINOKtrN        i-hO        aiHOOiONOCOOJINVCOOCN 
i-i  O  t-(  O  »-h  O  i-H  O  i-H  O  i-i  i-h  O  O  O  ^h  i-h-h  O  "i  O  O  »-<  i-h  O  O        i-<0       Oi-<00.-iOOOOOO  C5© 

co  CO 
■<r  co 

NMiOi|iMHONHSHOMMOJ<BiOOWMNO!ia<tiOM        OC  <N        WOCN^OTrMMNCINN 
CO  Tji  CO  •*  CO  -f  CO  ■«*<  00  "«*<  CO  CO  T»<  Tf<  rf<  CO  CO  ''J'  Tfi  CO  TJi  Tji  CO  CO  Tf  tji         CO  Tf         -W  CO  T1  •<*"  CO  T  Tfi  iji  tji  tj<  rji  lO  Tl< 

283 

COOOtO^COCMiOCOTfi-ilM-^CS 
CNTJ<                 Tt<^Hi-l          HNNNrt 

(SHOicOii'OcO'* 
CN^-I        hCNhCNM 

(30  TP         t--^         (M 
IM          05T»<          CN 

i-oOCMTjiosascocot^cN 

TH                   COl-H                   1-H           CM 

3SS 

O5O3  00 

ih  cn  *n  ■*<  "*  et  r—  os  »o  i-i  «o  >o  oo  o  co  eo  rt«  o»  ■*  cn  eo  oo  a>  *a  «©  n<      cjco     oo<Nt--'*cocN<cet^r-~cNi>ot-~co 

->*>  tt  lO  lO  -r  re  iC  CO  -f  i-O  CO  1  -  rt  ~  "0  CC  uo  t-~  C:  CO  ~  '0  I  -  -f  CO  l-O         O  i-l         rtHWtCOCNNCNCNHM 

cx>  OJ  oo  os  oo  o>  oo  os  oo  oj  oc  oo  oi  oi  ct>  oo  oo  oo  oo  oo  oo  05  oo  oo  as  os      os  o      os  os  os  os  oc  a>  as  as  as  as  as  o  as 

> 

z 

— 

a: 

§ 

0 

p 
IE 

1 

i- 

i 

0 

'-E 
c 
PC 

c 

c 

p 
2 

c 

pc 

» 

p 

c 

y 

p 

2 

c 

PC 

1- 

p 

c 

y 

p 
IE 

c 

Ft 

£ 

y 

p 

IE 

c 

— 

p 

c 
y 

p 
IE 

c 

pc 

C"- 

c 

c 
y 

p 

c 

1 

y 

p 

c 
pc 

B 

p 

c 

V 

p 
2 

c 

- 

p 

c 
y 

p 

2 

c 

- 

p 

c 

y 

p 

j: 
c 

pc 

p1 

c 
y 

p 
IE 

c 
PC 

p 

c 

y 

p 

2 

c 

PC 

p 

c 

y 

p 

c 

- 

p 

c 

y 

!E 

c 

- 

cr 

p 

c 

y 

p 
c 

pt 

p 

c 

- 

z 
pc 

r- 

_c 

p 

e 

- 

=  E 

c  c 

y.  y 

g  p 
lo'jc 

c  c 

E 
c 
y 

p 

c 
PC 

p 

c 
y 

p 

c 

- 

Of 

e 

c 

y 

2 

c 
PC 

p 

p1 

c 

1 

- 

1- 

£ 

y 

2 

c 

p: 

icv 

:i 

>.E 
h  c 

-I- 

i 

p 
2 

c 

PC 

p 

c 
y 

p 

"i: 
c 
pc 

i 

_p 
2 

c 

PC 

I 

p 
2 

c 
pi 

p 
p 

c 

p 
2 

c 
PC 

1 

p 

1 

pc 

I- 

p 

c 
y 

p 
2 

c 
PC 

p 
e 

p 

1 

PC 

c^- 

p 

c 

E 

2 

c 

pc 

1-HCO       loj1 

pj  pj  :  p 

c  o      c 

co  co        cr 

S  S  s^p 

2>S  e3  2 

c  oi  c 
P^PScop: 

!cn 

;  (=i 
;  o 

J 

o3,a 
is  ° 
ccpt5 

00     00 


NCC*iOCDCO     C35        O        i— I        l>-        Tf 
00  00  00  OO  00  00     00        0>        OS        00        00 


OS        ■*        H 


o    odd  dodo    o 
5?  ^^^^^^^  ^ 


C»  CB  » 


<B    ©       rO 


CO     CCOOOOOO     CO 

.  o  o  o  c  o  o 


o    o 


03         03 

d      d 
PQ     pa 


W     ^ 


U      S-.      t-     ^-.     tn      — l 

pp p  o  c  o 


O   O^^^^^^   OOP 

t^    00  CT>  O  r^  CM  CO  •*>     iO        CO        t^ 


<N  CN 


•8 

=3 

<a 

ri 

d 

d 

g 

2 

d 

pq 

PQ 

PP 

=3     «8 


o      o 


212 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


S 

£ 

$ 

t 

f 

g 

1 


•sjajxeq— ;onpoad  lei^rai 


•}8aj— T^dap  i^ox 


•»99j— todepno 


ran^Bp  8AoqB  aptvmrv 


•J88J— I8A9J 

■Bas   Aiopq  epmt^v 


pa^Bj^auQd  ssau^orqj, 


•^98;— do^  o^  q^daa 


1?  OX2 


o-d  o  «> 


COWMNtOrH 

05  Ci  CD  CO  00  t- 

oooooo 


t^  OS  t—  CO  Tf  05 

OOMOrtN 


1005NC010O 
OOCOtOrtCO 


03,Q 


tf    IPhPh&oPh 


1-H       ,<N00 


o  o 


+J  03  00  Oi'O 
CD  ~  ~  ..«> 
*~  S3  03  03  O 
rvi  C3  03  C^^ 

MASS'S 

Ommm 


NOOCU5N 


oo 


t-  Os  CO  CO  rt< 

ococo>roo> 


00000 


S8338 


i-H  i-H  00  OO  CO  00  00  C 
i-Hi-HOOOOO. 


•*lOOOit«OOlO 


OOiOOOOiOOOO 


i-H  .<N<N      .CN      .i-H 

q  ;  i  q  :  q  :  q 

o  !  o  o    .  o    ,  © 

a  :aa^a  -.a 


'cNOOCOOiaiaiOCOCO'^COCM 

I  lO  O  CO  CJ2  CM  < 

iOi-hOO-h. 


ONi*0>i0050>OOiONO<00 


aaaaaaa 

P5PhP2PhPhPhPh        :( 


aa 

:  :p5Ph 


a  2  ©  os  g 


lOiON  Mi        N     ^     00    NHOO*     CN 

lOOOO)  00         »     N      N     0005050     00 


eo 

CO 

«N 

* 

CO 

Tf 

c 

c 

C 

CO 

c 

2 

c 

s- 

OJ 

CO 

£   £ 


o    o 


q     a 

'■?     '■?      -d  »d" 

03  CD 

03  03 

Ph  Ph 


a  a 


do   ^ 

is  I 

PhPh    O 


o    o  o  o  o 


o  oooo 


*  *  *  ££*£  £ 

03  03  C3  03  03  ^  ^  ^ 

cq  M  cg  mm  of  w  of 

h  Eh  Eh  EhE-i  o3  c3  e3 

O*  d  d  do  cam  m 


h 


S    § 

a  a 


s 
l* 


2  3 

o  o 


:  :  2 
:  :  o 

.   .   © 

2  2*^ 
22  c3 
OO  Ph 


2  22dd 
u  ooww 


co  r-ooc»o 


•g  oooooooo 

*  3  3  3  3233  3 

£  o  o  o  oooo  o 

i-H  N     M     1i     U0COt>-00     CT> 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


213 


e 

e 
c 

i 

c 

: 

I 

'- 

s 

3 

'J 

i 

.  ;  ® 

i!- 

o  o5 

"5 

is 

GO 
| 

-d 

M 

c 

2 
o 

z 

I'd 

:1 

I'd 

-Hi 

O   03 

£s 

°cS 

I 

i-  c 

: 
■2 

z 

c 

o 

o 
o 

3 

833 

o 
so 

8§ 

o 

b 

ft 

Q.SP 

3 

OJ 

e 

OJ 

ION 
O5  00 

n 

O 

o 

CO 

s 

08 

CN"3<CO 

gg 

1^ 

09 

OS     ;00 

BO 

§8 

o 

-r 
C3S 

o    -oo oo t^    • 

tt>      -OS  cooo     • 

oo    '©oo    ■ 

— i  CO  ro  —  iC  cc  s  to  O  to  -o 

NOO<OWO(ONO)COMiO 
000>— (  i— iOi-iOOi-iO 

r^  oo  ■w 
>o^co 

Ol-Hi-I 

NOOCONWMOlHNtOOOMOi 
N^NHaiCCrtWOOOUOOO 
r-l--HOr-lO^HT-IOOOO0300 

NtOOSNOOOiW**NO 
OhOcjOiOhioOhN 
.-hO.-hO.-iOOOO.-hO 

OS-^OOCOt-OOCOJ      • 
00  .-1  t^  CN  t^-  •«•  t~-  CN      • 

OHOrtOOOOi     ; 

8 

TT 

s 

I'NtOKJtO'l'OV'* 
^1,<J*COCO'^CO'^t1'^1CO'**' 

CO  IN  CO 
rfi  00  CO 

(^5CNt^.CO>Ol>'-H05rOTtitNI^^H 
MONXO(OOCHO>OfflTliH 
COCOTCO-'S'eOCO'^fTfnjltllOCO 

OiOOOiCOCi-fOOTfiOiOCCO 

HCDCNh-MONH       ■ 
r-l  00  CN  t^  (N  CC  CN  N      • 
■*  CO 'Cf  CO  •V*' IC  O      • 

coco 

2£3?5S^  : 

3        • 

COiOCO"»ii-ir^cOt^.iOCO'<r<CNCO 
idi-iCN        NhN        CN 

lOHTfOiONOOOOOOO 
(NCNCNCN.-H        i-Hi-It-<        CO 

OOtj.  NTtNOOO      • 

HHCNNNH 

ohtmo'^ooi'o^n 
cn^hcoiooocoi^ocococo 

CT>0>0300000>0000050005 

t^CN— 4 

CO  00  CO 
O50000             • 

(OiOOOOOOOOONNOiOO 

toiocoaiMooaiNOOoi'^o 

OOOOOOOOiOOOOOiOOiOiOi-H 

iOhOIMhO<0000(OM 
Oi00CiCOCS'<J'00iOOs00cN 
00O100CT>00CT>O5O5O>00CT> 

(NCNOOOCOCOOCt^      • 
CO  i-l  "J*  OS  CO  t^  CO  00       • 
OOJCBKOOOO     ; 

c 

d 

> 

- 

pi 

Pi 

0 
co 

C 

'5 

0 

- 

1 
I 
IE 

o 

ss 

pi 

c 

V 

IE 

c 

ro 

a 

c 

co 

p 
IE 

c 

p 

c 
CO 

IS 

o 

1 
r 

= 

IS 

c 

« 

Pi 

c 

V. 

IE 

0 

p 

0 

% 

3 
o 

CO 

a 

z 

a 

£ 

0 

CO 

PI 

c 

<x 

p 

IS 

c 

- 

p 

c 

- 

IE 

o 
P3 

c 

i 

1 

p 

c 

g 

IE 

c 

OJ 

c 

K 

IS 

c 

<N 

P) 

z 
X 

p 

s 

c 

cc: 

PI 

c 

en 

p 

1 

c 

3 
IE 

c 

c 

PI 

0 

5 

IE 

o 

p 
c 

CO 

s 

s 

c 

p 

z 
c 

c 

1 

> 
-7 

> 

1 

x 

p 
IE 

c 

h 

z 

X, 

p 

IS 
o 

p 

- 

CO 

- 

s 
- 

CO 

% 

= 
IE 

z 

1 

p 
IE 

o 

re 

PI 

c 

CO 

IE 

i 

CO 

s 

CO 

Pi 

c 

CO 

c 

1 

- 

i 

CO 

= 
IE 

o 

- 

p 

0 

X. 

■=■ 
IS 

0 
:- 

CO 

PI 

z 

p 

s 

c 

p4  ^h  cm' 1-1  esi  co  ;  ;  i 

BCBacid  ;  :  : 

o  o  o  o  o  o    ;    .    . 

1/3    m    CO   t/>   OT   CO             .      , 

.s.s.s.s.s.s>;>; : 

oooooo«-;J3    ' 
P4«pr:tf«rta2c72    : 

OS  00      OJ  ( 


CO     CO  rr  O  iO        "V  CO 

O     O^  ■—  v  O  O)        Ci  3C 


o    o  o 

O     O       ^    ££ 

mm       a>     c»  o 
24    ^      fl    AM 

&£  S  SI 


z   z 


or     ,_, 


-c 


<N     CO     •     •     . 

.  o  o  o 

3  sooo 

s   Sooo 


12  z 


oo    » 
ZZ  •§ 


o    o 
55  Z 


22    2 


o   o 

S    9 


ad  W 
'El  S  "S 
oo  g 
DO  P 
o  o    ® 

SS     05 


WWW 


^  ^    ^ 


w    w 


^    o  6  w 
3  ZZ    o 

CO     PI  Pi 


CM  rt  Tji 


|  &    & 


sass 
3    •§ 


ft  aa  -g 

""    o       o 


W  mm  w 


11 


.^  .s     d  dd  •-< 

03  PmP3  o 


O  O 


o  o  o  o 

^  13 13  IS  13 


O  O      CB 

1313   3 


o  oooo    oo  ft 


o    o 


■§  «3^ 

S  >>>> 


o    o 


(MCO     -"T        iO     COt^OOOS        Ort     cN 


c   ^ 
<X>  CP 

zz  J 

I  Si  i 

|  aa  £ 

ft    05CQ    Q 


214 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sxaxreq— ;onpojd  vbiiiui 


189J— qidap  pno  i 


•!}89j— t^dap  no 


a) 

d 

o 

1 

I 
o 


S 


Tan^p  aAoqB  aptnijjv 


•%Qd}— \9A9\ 

B8S    Avoioq    epnmiv 


199J— 

pa^jjaued  ssau^onij, 


•;aaj— do;  o;  t^daa 


g  o  ©  03  g^ 
02 .2  «  >.2,£ 


oo 


cm  o 


^ 


ifltDOOOUJ 


HOlNO>N©tD^HMO!ONOOHClM(OiOrtO)rHOt<5 
HTf00«®OO>OONH«ir:c:-fO'XsC-*HC0Hii)00 
^rHrHO-HOOOOrHOOOrnOrHOO 


rHOOO< 


CO  00  <N  Tf<  iO  C<» 

co  tj<  co  co  co  -v 


OlHWiHCOf^MOlNO^OONOSOONtiiOCAHffiOl 
00«5HMMO)OOi05N<SHi1iCiOO)HHl(J(»®X>Oi 
CO■^■Wl■V■^,COrrcOCO'<3'CO•*l'^■<J'■«l<00'*|■^'<tlCO'*lCO'S'• 


0«5<00l 


O      -iCOiO 


'U50<0       -CO  O)       ■  rH 

•  t-ii-h  -corf     .CJ 


lO      "iC      'OOlO 


ioocoocojo 


OOOiOMQOHHONONtOOiONHON«NO!«' 

;     :ilOiHMNNiOrtNNN«N'!fif4!OONOl 

0)0)0)0)0)0>0)0)0)0)00)0)0)0)0)0)OiO)0)0)0< 


rHMMlOl 


rOrQ. 

o  o 

PHrM( 


g  g  a  S  :  g 
3333  ©3 

O  O  O  OT3  o 

CmPhPhPh  :« 


NhNcohNhN 

.oooooooo    ;pop 


CO  rH  CO  ■ 

fH  a  fl 


</)        wmwKtnwtflco        w  w  w  m  w  [/) 

S  '2SSS9SS9  -SSSSS9 
'jo  o  3  3  rQ  3  ic  3  3  3  £  3  3  3  3  3  3 

cd  O  O  O  O  O  O  O  OT3  o  o  o  c  o  o 


1 

a 

ft  ■ 

03  O 

£55 


•j3  o 

CO 


rH      (N  ( 


C<1     iO     Is-     r- 

N     N     h     N 
"O     iO     iO     W 


8      S3      Si    S3 


rH  rH      <N 


lO      OS      CO  "9<      rH 

6    6    6  6    6 
55  £  5555  55 


03  (X>  <U   ©  <D 

o  o  o  o  o 

o  o  c  o  o 

W  W  WPd  W 


55  55 


ON         rH         CO  tj< 


55  55  55 


.3  .3      .a      S    S 


3  a  £  £  £      £ 


o 

o 

0 

o 

55 

55 

55 

fe 

3 

Si 

53 

-. 

PQ 

W 

M 

pq 

o    o 
55  5? 


Q  O 


w       °       °    ° 

o 

o 

2  3  33 

rd 

rd 

o  o  oo 

o 

O 

rtflfl  a  a     a     a     a     g   g 

OOO  O  000         00303 

.M   .S3   .S3  OT  .OT     .OT     y      »     fl   ffl 

.2    .2     13     t3     i3  &  fa        fa        fa        fc'd'O' 

rtrtOOO  O  OOOOoa) 

oos^  a  aaaa«« 


lO     rH  rH 


CS      CO 


<N         CO 


Ifl 


H 

I    55 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


215 


7 

- 

X 

—  _ 

i  i. 

i. 

cy 
a 

r 
8 

-2 

CO 

_g 

'3 

3? 

■    '"3 

:  :£ 

J  j| 
i©   ;  oo 

IS! 

"3  o"5 
x  O  x 

- 

i 

- 

1 

1 

C 

- 
O 

5 

0 

X 

= 

03 

c 

x 

cr 

- 

X 

"3    ; 

^  : 

©    ■ 

<s  • 

c    .' 

©  o 

11 

P   C3 
X 

o 
"UK 

s^s 

11 

3.CG 

>. 

>> 

t-i 

Q 

ft 

co 

1 

HI 
CO 

OS 

X 

EC 

1  - 

s 

5 

IT 

r 

CO 

IC^OOOO  OO-h  C       ooo 


i-hOO^OO— (  o 


ITPOC^HC 

I  CO  ^  »-l  t 

lOt-H  »-l  < 


!  re  "-=  X  l-  —  I r  ■—  I  — r  c  c  ri  /  - 


CO  tj<  rp  -^  rr  ■ 


N  ffl  LO  X  w 
CO  -^  CO  CO  -^ 


CO'*l'<3i-^CO-^TrCO-^''^COTrCO'>3'CO'^ 


l-  co  lt:  i  -  cm  x 


00  O  CO        CT>  ■ 


'3S 


uJXCNOHJIiOMNhh         CO  I~  Ci 
00  T  t^  co  co  co  CO  CM  O  X  X        CM  l~  CO 

00  C>  00  O^  Ci  C7S  C75  CCi  Oi  GO  CCi        CC  Oc  CT. 


O  CM  O  O  O  00  O  f 
CO  T  CO  X  CO  IQ  cc  o 

CC0101*C10XD 


•  l~-  cs       >-o  CM  ~ 


co  c  cm  i.o  co  c  io  >a  w  co  co  —  x  co  co  .-i 

X  Ci  X  X  C3        X  ~-  Oc  CC  X  O  Cc  X   — .  O.  X  CO  X  CO  OC  CO 


tH.-O^M-hM 


co  oo 

9  9 

o  c 

tftf 


B  £  C 
ooo 

CO    CO    CO 

.9  9  9 
333 
coo 


n  c   .  a  ace 

o  o    •  o  ooo 

CO    CO        ■    CO  CO    CO    CO 

g  a  ^Jj  sag 

3  o  3  3  c3  3  3  3  3 

cd  o  o  H  c  o  o  c 

pi    IpSpJcop;  tftftf 


>  o  o  o  o 

3    CO    CO    CO    CO 

:  c  a  a  0 


r-HCO 


i-l  CO  .-H 

CCS 
ooo 

CO    CO    CO 

fl  q  c 


i  CM  CO 

I  c  c 

:    C   C 


33333333  ,£* 3  «  333  !?3 

CCOCCOOO        O  OT3        c  o  O  H  c 


ItfcO 


5  5  5 
3  3  3 
c  c  c 


rtNHCCrtCN 

CCCBCfi 
c  c  c  c  c  o 

y:   co    co   co   CO   CO 

C  C  C  C  C  fl 


X2r      . 


-^       CM    o  xo    o 


■^h  CM     CM  -h 


TMMCO     i-l 
CO         .      .      . 

.    o  o  o    c 

I  £££  ^ 

,_.  33V  3 

5  as  a  a 


o 

o 
2 

o 

g 

CO 

CO 

w 

CD 

w 

w 

3 

3 

3 

5  £    £    £ 


£  £  £ 

ffi    w    w 


•a  -s 

C3        cc3 


©  ©      J=X&      A 

P5    a  ooo  o 


C3      S 


3     .§     5 


s  s  s 


1-1  CM 


216 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq— pnpojd  psi^iui 


•^j— t^dsp  ib^oj, 


•}88j— qidap  no 


•%qq} — etrejd 
ran^p  8Aoqe  epnmjy 


■B9S  Avopq     apn^i^V 


"\Q9}—dO%  0%  T{%dQ(J 


g  oi  c3  fl-g 

oa.2  «  ^.2.2 


CNiOOOcOtj<.— ICONIC'— I 

■*  00  to  00  CO  00  lO  OO  iO  O) 

<-<O^HO--lO.-HO.-HO 


CxSTflCO^COT^CO^fCO' 


>0  CO  iO  00  r»  lO  CO  <M  ■*  ( 
H^(NMcNCOrtCOrt! 


COWiOOOWNt(ItI<00 

cocMcocNcvio-fT-icNoo 

00O500C500O500C50000 


^HCMrHCM^CM^HCM^HCM 

oooooooooo 

OOOTOOC/>C/}CZ>CZ>C/)C/3C/3 

gggggggggg 

2  3  3  3  3  3  3  3  3  3 

OOOOOOOOOO 

tfpqtftfP4P3tfP4tfpc5 


88 


OOrtOOrHCOTI'lOXlO'S-OOOH'VXN'fOl^fO 
lONNCOlCNOCONXlCNCOOONNCOOOCNN 
,-HOT-trHT-lOt>).-l.-l©i-HO.-HOOO,-lOrHO 


CQ-*l<C<5COCQ*&C<iCOC<i**<m-<Pm-*<-&-W}-rPCO-<# 


.-HOI       IrH 

pi  pi  :  p)  c  pi  ;  pi 

o  o    .  o  o  o    .  o 

00   CO       .    K)    00    00  oo 

.s.a>>g.a.g>;a>*s.g.s 

,0,003,0,0,003,003,0,0,0 
OOJ-'OOOHOHOOO 


!§§§ 

■aa" 


ItNCO       .HtNrHtN 


ca^i^i^  ct^j  oa  ,s-;  ,u  ,i_2 
oo*-000£0_f-:000 


sis' 

333 

o  o  o 

tfptfpH 


;  g 
c3 
■Cc 


g  pi  g 

333 
o  c  o 


§  s 


CI     CO     CO 
N     O)      N 


o      o      o 

£   £   £ 


£     5? 


pq     pq 


CJ  u  ^  W            CJ      ^.       ^, 

°S  "C  'C  °£          'fl      <*H      ^* 

'©  '3  'S  '© 

£  £  £  £ 


£  ^  -3 
£  a  a 


B    W    M    M    M  ai  a 


a    S 


rt      tN  CO 

o  -<  <n  6    o'  6 

^  6  6^^  ^ 

a-  £  fca-  --  s 

©  ..  „©    ©  <» 

£  •§  ££     £  £ 

c3  g  g  03   c3  c3 

S  CO  COS     8  S 


M  M  M 

co  oo  oo 

"3  "3  "3 

,3  ^  rf 


■§  w  pq    pq 


03  O 


So 

2* 
m 


A* 


•3  ^  ^ 

s  §  a  a  «  « 


pq  pq  pq 

'O'       'O  'O'  'O' 

©         ©  ©  © 

PS     Ph  tf  pq 

»      *  in  to 


pq 

-r)  .2  2  2  .2 

©  3  33  3 

P3  O  OO  O 

r-  oo  C350  —i 


BLATCHLET] 


TABLES   OP   WELL   DATA. 


21' 


- 

i- 

c 

}E 

c 

c 
— 

c 
- 

c 
- 

c 

c 
- 

oo 

l! 

© 
*~"e3 

05 
CO 

o 

si 
as 

1 

s 

- 
a 

a 

i 

X 

T3 

% 

c 

1 

c: 

-s 

■c 

1 

■- 
t- 

c 
2 

c 
or 

'- 

O  'S' 

n 

CO 

§        «0        CN 

I 

CO  CO 

§s 

I  i 

•=>  : 
x  : 

o> 

§8 

00 

OJ 

IO        if 
IO        IO 
00        00 

o> 

IO 

3 

23 

05  0) 

aa 

8 

93 

KOHioCiNM^fflHCO        CN        t-H  05              O5>O00<O 

te  oc  i  -  m  oc  t>  io  o;  io  io  co      io      co  oo           tj<  co  i-i  co 

_lO  i-H  -HOOi-lOi-1  .-4.-I           1-H           1-4  CM                   O  O  — 1  O 

NWiOHOiOCONOOOONOiOOliONM© 

IO  »  (N  X   •-   O.   t~   ~    ^CCNHfflrHlCi-l^iH 
i-lO^O-HOOCNOr-I^H^H^H^HrW^-lr-H-l-H 

lOi-H 

o  io 

t^0010rHCOM«Tj<OJN         00         OS  i-H                hlOMtII 
CO  -tf'  -W  CO  i— l  CN  **i  O  if  Tt<  CO        -f        CD  i— 1               IO  CD  00  CO 
CO  •<*>  CO  CO  "<«4  if  CO  if  CO  CO  CO         CO         CO  CN                if  "f  CO  "V 

OONlOOOlONOCNOHWOWrtLOWN'')' 
■O'Ot^rtTrOINaOO'^NCiKK'fl'ML'5  00 
CO^CO^<CO-<fif<NifTfCOCOCOCOCOCOCOCOCO 

CO  00 

NOilNO       "00 

CMi-icoeNi    ■ 

00  CO 

I-H  CO 

oo 

os00           3 

eq 

OiO00NO>0»N00iONOt0Ot^Lt)<0OO 

CO  IO          CM  if  CM  1-H  1-H  i-H  r-l                  CO  CN  "91           THTf 

II 

if  t-  rt>  05  IO  I*-  IO  iO  -f  *<f  CN        CM        0)0              OVON 
^  —  CO^CT.  O-Hl-CNCNif        cm        ^n  o               TMOOC, 

00  05  00  00  00  03  00  00  00  00  00      oo      oor-          osooooi 

x  r~  co  o  >a  o  iQ  cm  co  10  10  c—  -f  10  i-i  l-  ro  io  b- 

"   ~   -O— c^r-HCO'— i— (-HLOOCO-TCsiCOicOOi 
000000O300O5O500O5O30000O5O00000000000 

c 

- 

i 

1 

i 

■r 

p 
c 

c 

p 

1 

pi 

f 

c 
[/ 

p 
IE 

c 

pi 

c 

D 

F 

c 
c/- 
F 

1 

- 

i 

D 

IE 

c 

- 

i 

i 

pd 

0- 

§ 

p 

1 

pi 

1- 

p 

c 

■s 

p 

1 

pi 

s 

C\ 

p 
c 

Of 

p 

1 

Pi 

p 

c 

c 
c: 

€ 

1 

I 

« 

c 

c 
a 

1 

PS 

c 

p 

IE 

c 

p: 

s= 
c 
■J 

I 
IE 

c 

p: 

i 

1 

pi 

i 

p 

1 

CN 

p 
c 
a 

c 

Pi 

1- 

i 

g 
1 

Pi 

re 

§ 

S 

c 
P4 

1 

p 

IE 

c 

Pi 

6> 

i 

c 

c 

1 

Pi 

p 
c 

■J 

IE 

c 

Pi 

!§ 

H  C 

cs 

i 

I 
IE 

c 

Pi 

T- 

c 

c 

F 

IE 

c 

P= 

> 

h 

X 

Cv!  i-l  CM  i-H  CNI  lH  CM 

o  o  o  o  o  o  o 

CO    K    K    K    CO    CO    K) 

C  C  C  c  g  c  c 

IE  IE  '2  IE  IE  IE  |S 
o  o  o  o  o  o  o 

O.  5D  CD  CD  00  CO     t^ 


CN     O     iO 


IO      00 

o    o 

IO     IO 


• 

00 

CO 

IO 

CO 

•     i-4  CN  CO  Tt<  iO  t^ 

d    ci 

o 

o 

o 
2 

o 
2 

•    c 

c 

.2 

z 

2 

c 
2 

c 
2 

c 
2 

pT  pT 

a 

a 

pT 

pf 

o  pi  pi  Pi  pi  pi  a 

^  s  a  a  s  s  a 

s  aaaaaa 

g  Pi  3  pi  S  pi  Pi 

P  OOOOOO 

c3  o  o  o  o  o  o 

S  QQQOPQ 


a  a  a 
a  a  a 

pi  pi 


ll]     M     t 


fc     5? 


o     p     q        +j      +j 


fi    fi 


Pi     Pi 
o    o 

«   ft 


o    o 
53  53 


o    o    o    o 


^-^-72 


o  o    o      o  o  o 


Pi    Pi 


P  0 


O3o3c3c3>  ^^^ 

Q  O  Q  p    i-i      ,-,•    (_;    ,_>• 


iiotoNooa 


CN     ?5 


CP  CP   CP   Q?   CP   CU 

x  n  x  m  j*  m  g  g  pi 

_C3  _C3  _C3  rt  rt  _g  O      O  O 

la  ^^i6'?ii  S   ci  c3 

5  ^^^^^^  S  a  a 


a  : 


o  :q 


o  -o 

c!  °  c  ° 


.23  .2  .S3  'C  Pi'C  C 

t-4  u    im    S  cp  S  cp 

o  s  s  aaaa 

a  s  s  ■<  < 

CO  ^4      IO      i-4^  C5  ^ 

CM  <N     <N 


o    o      o 

13  13    13 
o  o    o 


2  2  2  2 

13  13  13  13 

o  o  o  o 

f  IO  O  N 


218 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq — :pnpoad  p3i;nii 


•^89j— q^dap  pnoj, 


•^99j— i^dap  uo 


ran^p  8Aoqi3  apnmjy 


-188J— J8A9J 

•B8S    Aiopq    epnjijiv 


•}88J— 

pa^a^uad  ssamtcnqj, 


•}89j— do;  o;  q^daa 


3  oi  eb  £"£ 

»5  ®  ''.S  ® 


OQ 


lO  t-  OS  i— I  lO 

iO  rt  lO  10  i-l 


lO  CO  i-(  OS  iO 

if   00  Ttl  T*l   00 

CO  CO  CO  CO  CO 


Is-  IO  ■•*>  OS  «o 

rtHM        i-t 


CO  i-l  l^  00  ■<*< 

IO  OS  Tf  T»i  00 

00  00  00  00  00 


i-i  (N  , 


,  <N 


a  a  d     a 

o  o  o    ,  o 

9I99  :| 

Id  3  Id  o  3 
o  o  CC  o 


o 


f-nOi-n-HrtOi-n-i'-HOi-ii-iOOO 


'XMMtOO-tiOCONrtNCOO 
'O5^00'*1<00M>rHT)100(Nr-liH 
COCOCOTt<COCOCO-^COCOTJ<Tji-^i 


iio*Hoo»oi 


OOIOOI 

1-H  HlOl 


000000OS000000O30000OSO3< 


(Ni^C^COi-l<Nr-ICOrHCNICp 

1  9  3  E  9  9  .9  .9  .H  .9  .9  S  .9 .9  • 
'  IS  "3  IS  IS  IS  IS  IS  IS  IS  IS  IS  IS  IS  o  o 

■0_mOOOOOOOOOOO*CO 


CO  CO  COCO  CO  CO 


MCMONN 
<M  CN  OS  TP  00  O 
00  00  00  00  00  OS 


hNhNM 

fl  fl  C  fl  fl 
o  o  o  o  o 

K   W   K  M  m 

a  a  a  a  a 


£  o  c  o  o 


COIM 

coco 


i-H  <N 

pi  a 

o  o 

.9.9 

rD,D 

o  o 


00      N1O00OS      00 
OS     OS  OS  OS  O     OS 


00    o 


pq   pq 

.   ~      6  o    o 
P3  «  pq  ££  £ 


oc 

if. 

re 

o    o 


-D     D 

9   9 


^      C3  03 

3      CO 


i-l  W     rtM®N     * 

6        6    6  6  6  6    6 


05       fi)   CJ   0^    (^       Q} 


5?  £ 


WWW  do  o      £     £     £     £  ££££  £ 


£    £  £ 


pq  pq  pq 


pq 

__,     _j     „_,      o  O      O  _. 

rj)      fl      ^|      .H.rt      ,h  r^ 

a>    <o    a>    ^5,d    ,D         ® 
tf   K   P5   OO   O       PS 


o    o  o  o  o    o 

IS  IS  IS  IS  IS  IS 
o  oooc  o 


_M>       M     St) 

§  3  S 

o    o  o 


a  o 


•j3  o 


N     M     f     "OtD 


i§3c$8  s 


BLATCHLEr] 


TABLES    OF    WELL    DATA. 


219 


-- 
- 

- 
I 

5 
qq 

i 
b 

B 

0? 

T3 

d 

a 

0? 

-3  J 
|1 
Bcn 

—  00 

s3~ 

| 

-r 

a 

0 

X 

CD 

s 

1 

09 

03 

® 

US 
x 

3 

0 

Gas,  874  feet 

Gas,  880  feet 

Gas,  878  teet 

Gas,  897  teet 

—  1- 

o 

o 

c 

CO 

ooooooo 

Nxmocoo 

i-l         l-l  rH  CM  rH  CM 

o 

C 

5 

— 

o 

C3 

= 

s 

8 

05 

Oi 

o 
— 

00  lO 

oc  -< 

coo 

CO 

So 

o 
oo 

o 

00 

a 

X 

O  0C  O  f  TP 

00OGON 
00  OC  00  OI  00 

X 

gl§l 

T 

■- 
- 

cc 

K 

1 

L- 

g 

0 

x 

it, 

c 
r 

i_: 

g 

1 

» 

X 

[- 

x 

-.- 

C 

1  - 

I- 

- 

t; 

— 
x 

9 

— 

QC 

S 

/ 

HlflNC 
CC  CM  t^-  CN 

5 

CM  io  r--  re  O  « 

| 

WfflHCO© 

oonHir^c;sNTPic^-;i- — r  n  m  fu — -rcr;c 


^  O!  h  ^  m  ?.  l:  ?;  c  l^  h  c  c  ei  ( 

CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  ^1  CO  CO  ^  CO  CO  M1 


i^l'NM 


NONCiO^NXNO. 


!SS 


Oi  oo  co  r-  x  O  c;  oC' 


■«}<  oo  O  oc  irt  ^h  rr  t^-  f-  o  x  cm  lo  ci  [^  co  oc  -*  >o  oi  ■-  -jz  r-  —  r*  — <  i o  co  t -  cm  x  co  i  -  i-h  i~-  co  r-  t-  r-  o  x  cs  cc  cc  cm  c  c  cc  re  —  cc  — 

00MOffl00O»M0100KC!X00M010CaXXXr.MC0!XZi«W00«MaXM00  00  00  00X»0CtCXX0,.KK010CKfll 


o  o  c  c 
oq  cq  on  03 

S  9  9  5 
2  3  3  3 ; 

o  o  c  o 

Pipipipii 


ccaac 
c  c  c  c  c 


>CMCO 

:  a  a 

I  c  c 


.CM  CO 

:  b  b 

.  o  o 


o  o  o 


-1  ,C 

0   0 

«P5 


—  c 

:p3 


3  ea22 

CHOC 

tf  to  Pi  Pi 


.CM  CO 

■ii 

~   C   C 

co  Pi  Pi 


,<N,-<CM      .CM.-ICM 


j§ 


S  B 
o  c 


DO  Pi 


,0,0 

0  c 


Tie 
X- 


o  o 

Pi  Pi 


O  O' 

Pi  Pi 


,rH    ;cm 

■  b  ;  b  :  b  b  b 

000 
k;  K!  a: 

b  :  b 

o  o  o  o  2 c  3 ©333 
"cccc  cc  cc  ceo 

:  :  :  :pi  :pi  :pipipi 


o  c 

Pi  Pi 


CO      CM         CO  t^ 


N     1C     W 
O    Oi    o 


t~  CO 


■a 


05 


M 


1-1     CM        rt 

6         6       6         6       6666      6  65 

,B           X»        ^           ^         fl      ^      ,£|    ^      ^  ,B°) 

600            M          CO            UO          bo       W)       W)     bX)       tvo  bfl          p, 

I     M.  .?^^^  S    J 


53     ^ 


i-H     CM  CO  t»<  t^  10  CD 


00      •<*!      CO 


z  zzilzzz^  ^  ^  ^  &  ^ 


<B      41  ©»«  (C 


i^^^X!  fl  ^  fl  ,C  ^ 
fe  >>>>>>b£b0b0b0b0bC 
O  OOOOCOB  B  B  3  B  3 
El,     fe  Ci,  fi,  ft-  fe  Et(  B     W    W    W     W    W 


i 

i 

g 

% 

B 
C3 

s 

B     B 

C3      03 

| 

g 

bo 

bo 

bo 

bO 

bo 

M 

bo 

bf 

s 

S 

S 

§ 

s 

3 

s  s 

§ 

§ 

=3 

■9 

=>} 

>« 

«8 

=3 

=<3   ^5 

=3 

c^ 

TJ 

>g 

m 

tJ 

T) 

•rt 

-3    -3 

-3 

T) 

Fh 

O 

O 

0 

0 

0 

C 

b 

^ 

t 

£ 

iS 

* 

^     £ 

It 

f5 

rrt 

c3 

03 

C3 

C3 

c3 

C3      C3 

C3 

Ifl 

s 

t-, 

U 

O 

O 

0 

CJ 

O 

O     O 

O 

O 

O     P- 


£     .5      ^ 

-3      "3      »d 
W     H     H 


B  B  fl  B  B  B 
000000 
co     m     co     ot     fi     m 


o  2  2  2.2  2  2 

2 332233c 
o    " 


b   S  65 

000 

000000S S^SS 


-f    UO    o   t^ 


OS  O  —iCM 


Sc5! 


220 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siajjeq — ^onpoad  rBiitui 


•%&}— TU(R>p  ys%o  jj 


188J— q;d9p  no 


inrn'Bp.9Aoq'B  aprimiv 


•^99J— I8A8I 

■B9S   j&.o\dq   9pn;mv 


■J99;— 
pg^BJ^gugd  ssaa^oiqj, 


•^aaj— do;  o;  mdaa 


3  2.2  f3  S« 


az 


Gas,  935  feet 

Salt  water,  965  feet 

Gas,  945  feet 

Gas,  950  feet.    Salt  water, 
977  feet 

a 
a. 

i 

ex 

I 

c 

' 

a 
a 

T 

9 

a 
0 

!S 

"ei 
rx 

8£g^ 

00          NH 

?; 

o 
o 

o 

OO 

CM 

OC 

oo  os 

HOOiOH(OOiOIMiO[^OOOOtD»OHiOOCOO' 
OOOlOWOOlOffl(DOHCOiiOOr/'NiOr-lOOl 
i-HOi-Ii-<t-I,-I,-IOi-IO»-(OOi-I©i-Ii-I©i-Ii-I< 


tocoo* 


OlNiOO) 


lOOOiOMNINVNOaiOONOCI'l-X' 


©  lO  CO  < 
<M  CO  <N  ■ 


OOH(OCOOOiO»0)l-OONN001iOO(NiOtDOOHNO 

HOO)fflo>0'»OMOnO'*©ci^'*niooM»'*nio 
>  oo  <-  — 


OO'OMOi 

CO  00  CM  CM  o  i 

00  C5  00  00  00O3  00  O  00  O  00  ©  ©  OO  ©  0000  ©  00  ©©  00  ©  ©  ©        O0O0©00©< 


52  © 


HNHINHINCONCOCliHMHNMHCO 

ooooooooooooooooo  , 

.2.9.9.9.9.9.9.9.9.9.9.9.9.9.9.9.9  :  : 
w  2  2  2  2  3  2222  2  2  2  2  2B32°5 

'C  ooooooooooooooooo  "O/Cl 


CM  CO  >-l  CO 


O  CO  O  CO  OOOOOOOOOOOOOOOO  O'O'O        o  o  o  o 


00     00     o 


o  oz 

55  £   - 

c/3  tzi  a) 

2  2d 

rd  ^o 

W>  tUOrt 


o  o  o 

££  £ 

'a  a  a~ 

MA  rd 

o  o  o 

a  a  a 


M     N     to 


I  5.  ^  *  5-  *  ^  I  Ifc  I  »  fc 

"    is  j§  -g"  -gV  ■g"  g~  g~ 

g<     g<     rt      &«  C3  .0     .3 

Q     g     fl     fjfl  pi  oo 

i      cj    ci    o    oo  o  fl    fl 


fl    ft  ft  ft  ft 

s  a  a  a  a 


o     o  ^  ^  ^ 
.23  .23WPQW 


o    o  <u  a)  <u    ,d      ,d 

N     OOOiOH     IN        CO 


■a  -a  -a 


■h  "d  t)  "d  ^ 

,£4  <D  »  tt)  ,Cl 

Q  tf  tf  tf  Q 

^  iO  CO  h  OC 


2  2  2  2  2 
2  id  3  23 
o  o  o  oo 


.a  d 
o  o 


BLATCHXEY] 


TABLES    OF    WELL    DATA. 


221 


gpq 
O 


°8 


:3a 


70 
o 
o 
eo 
u  o 

53 


~  c 

CO 


t~-  Oi  O  r-  CO  O  O  CO  CO  i-H  m  OS  Oi  Tfi  CO        CO  O  CM  ^H  CO  CM  00  CN  CO 

ONNCSOOCOrHOO^NrtOO-OiHOO         00CO^COt~-i-H^H00i-H 
»-H  O  I-H  O  O  1-H  i-l  >-H  ^H  ^H  1-H  O  -H  i-l  ^H  .-H  t-H  t-H  fH  1-H  i-H  rt  ^H  i-H 


NOHOOH 


X  3C'  a  rt  00  O  ' 


O  t>-  COCO  i-H 
00  O:  i-h  00  CO 
.-H©»00© 


COHOCO^OO^TjifllCOHHtOE 
CONOOOHTrOHOONOOrtCClOOH         HNCMcONCCOOrHOO 

co -hi  eo  ■*  ui  eo  co  co  co  eo  co  ■*  eo  co  co   eo  co  co  co  co  eo  co  co  eo 


1-H   t^   C~ 

CN-HOO 
CO  CO  CO 


CN  W  CO 

;8£3 


lOi-H. 


i  CN  00  <N  T  < 


eo  cn  ■ 


'  1<  OO  *  iO  U5  O 
00  CT>  O  CO  " 
i  00  00  OS  00 


00  00  00  00  00  05  00  00  00        00  00  00  00  00  00  00  00  c 


CNOSOtNOO 
00  00  00  00  00 


CN  CMOS 
00  00  00 


ooooooc 


00  OS  ^f  OS  OJ 


<NCO< 

o  o 


.CqnNMHN 


as  :asaja§aass 


9  •  9  9  9 

o  o  ot ooo^o 

PhPhPh       iPtfpHpHCGpH 


.0,0.0 

o  o  o 

PhPhPh 


,0,0  03 
O  O  Jh 
PhPhCO 


CN^H  CNi 

a  a  a 
o  o  o 

ill 

o  2  3  3 

»o  O  o  o 

:phPhPh 


S  9 

S3 
o  o 


ICN 


l  CN 


~  >>p 

to  <-  o 

:«3Ph 


a  :  p  a 

o      o  o 

1/5        .    CO    CO 

.9  : 9  a 
3 ,2  3  3 

CO  o  o 

Ph  :p3tf 


.-H.-HCN 

a  a  p 
o  o  o 

CO    CO    CO 

pi  g  g 
333 

o  o  o 

P-PhPh 


.<N    .cseo 


Is 


coPhPhco    IcoPh 


J2^' 

o  o 

PhPhC 


!«Ph 


00      tlON      lO 


00500     CT>        OS  O  OO  O        OS        OS     O     O     OS     OS 


»  1(5  lOfl  «  CDOO  15  r>Nl 
O  O  OO  O  OO)  O  OOc 
IO     io     1QU5     "5     Htfi  ill     IO     IO  IO  • 


06660      6 

53  £5353  53   53 


o    o 
53  53 


53  53 


o    o 
53  53 


53  53 


pi  p  p  p  g 

,p  AAA  g 

0000  5 

p   pi  a  p  .9* 

ep     a)  ©  <d  P^ 

Ph    PhPhPh  CO 


000 
5353  53 


9   9 


Ph    Ph 

9   9 


Ph     Pi 

9   9 


►  *  *  fc  £  fc 


99   9 

COCO    CO 


Ph    Ph 


.     ,  ,  ;    .  09     . 
00000  ££;    o 

53  53£53  £  22-  & 

CD      0*  CD  CD      CD     '3*72      05 

.a  .p.p.p  ,3  SB  a 

©     COO     O    •—•-j     o 

S III  I  ^^  s 


G 

.  o 

•S-S  «8 


•8  «« 


XJX2X5 


0  -a  -a  -a 

»3    3    S    5 

a,  P5  P5  PQ 


o  o 


O    ^^^    Ph       Ph         Ph 


Ph    Ph         Ph       Ph 


pa 

co   'o'   'o'   tO   #2   «   -2   ti 

©       CD       (»       <»     fl     ,£3     ^0,       CD,n     ,m       1-.    w       w       ^,ih^-(     ^ 
Ph    tf    Ph     Ph    O    O    O     PhO    O    fip    Ph     PhOO    O 


II  S  a 

PP  «  w 

^^    TO    TO 


PP  ^  ^ 

111  1 

PP   M  hS 

•a-a  -g  g 

2  § 


85  88 


eo 


i-H      CN      CO 


115      O     NOO 


Oi-H     (M     CO 


1  IO      CO      t^  00 


222 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


•siaxreq — ^onpoad  i^nini 


■%wi— q^dgp  p^oj, 


g  :8 


8  :g 


COIN 


T3 

pa 
.2 
d 

o 
O 

I 

■■7- 

§ 

o 
Eh 


•%Q9l— q^dapno 


uin^p  9  Aoqu  opn^i^xv 


N»tCHtO(N05(D(Ol'CO(NOm«iOCiH(NVOlOlOMNtC( 
HMOaCDSCOC^CI-  i-  C  C  C.  C  (/  I-  rt  rr  a  !D  K  C  ( 
»OOOOOOOrtOi-tO^-iOi-iOi-iO^HOi-H^-i>-iO^HO»-i< 


<r  an  **■  «c  t» 


199J— J9A9I 

B9S     Avopq  gpn^i^xv 


^HMOcoOMmcorortmcoTrcorortvHNaiooccHMrtTtNviCN 

I    ^  ^  Tf1  M1  ^  ^  CO  ^  CO  ^tf1  CO  ^  CO  ^  CO  ^  CO  ^3*  CO  CO  CO  ^  CO  ^J1  CO  ^f*  CO  ^^  CO  ^*l  CO 


190J— 

pg^j^gugd  ssgu^oiqj, 


IINllrHMrHHCO. 


•^99}— do^  0}  q'jdga 


-rXOlceOJ00O300OS000000O500O50000C)0000000000000OS00000CO500OJ< 


oqco<Ncoi-ico^-icortco^HCOi-<co'-ico>-H<N^H(N^-i(N^-i<Ni-ico 
oooooooooooooooooococoococ 

999.9  99999999999c9999999.9  99 
3333  3  3  3  la  3  3  3  3  3  3  3  3  3  3  3  333333  3 

oooooooooooooooooococcoccc 


J.9.9 

133 

o  o 


o  c  o 


3  1,2  «  S  « 


Sfc 


'•^5 

CO 


cq     PQ 


CM         CO         Tf         IC         CN 


E  £  £  fc 

t£  >;  >^  >; 

(-1  fc-  U  (H 

h  h  fn  h 


£  2 

iH         CO         »-l  -- 

CI  Pi 

5    5    5ft  ft 

55     fc     fc     £•  £• 


a  a 


o      o      o      o 

3    3    3    3 
o    o    o    o 


pq     pq     tt 


3    8 


o    o 

rQ         ro         --J      -^ 

fi    Pi    oo 


^ 


BLATCHLEY] 


TABLES    OF    WELL    DATA, 


223 


1 

J 

0 
>~. 

oc 

a 

3 

C 

1 

- 
a 

a 

■5 

a 

00 

Gas,  954  feet 

Gas,  865  feet 

Gas,  855  feel 

Gas.  943  feet 

3 

0 

s 

OS 

~'~ 

-- 

i. 

0 

-a 

§ 

co 
C 
+a 

£§ 

Ph 

03 

Ph 

> 

CO 

5> 

M 

oo 

3 

Tl 

03 

r. 

OS 

t~-      -CM 

O        -OS 
OS      '00 

11 

p 

X 

e 

00 

X 

a 

X 

IC   K 

OC  0 

0 

owe 

-  e 

—  x 

00  X 

S3 

coco 

CM  — <  cr  X  t^  :r.  CN  X  l-  ~  -r  t-  i-  i^  i 1  t^  re  ~  X«Krr/.KXM?lSN-'rN«ciN       -r  K  K  l»  -  y.  ^  C  -  oo  co  —  co  -*r 

fl  ro  N  ^r  N  -  ?)  C.  1-  rt  ^  re  rc  r  re  /.  «  C  /.  x  S  i"  -  ^i  t r  L-Nc;-r~:M~:-rl--        o  re  t-  ue  -r  -r  CO  ie  *r  c.  —  t-  ce  io 


^H  -H  lO  ^H  rt  O  . 


coroicocoicO''j<coco 


+  ~ 


cOTrocereoo-^rMMcCL.ecorccc.i.ce^-^'^Trerc' 


MM^'KrK'!rM«Tr<»«M( 


coin     -^h  cm—ho    -coi-h 


CO  O  O  X  —  :~  ^•CC-iNeiNLOt--r:CT  X  X  C  t  l:  OiOOOOOU5N»OH«0  WOOOONOlOgOONMOH 
-o  co  -x  re  <-.  co  co  x  o  co  —  -r  -r  re  —  ~  ■-  r-  —  —  x  re  -r  co  —  —  re  —  x  re  •  -.  co  i-  —  O  —  >-e  -r  o  —  re  re  —  cm  —  x  re  —  ie  re 
x  x  -a-  x  x  -r  x  x  x  x  -r  —  x  — .  x  x  x  x  x  x  x  x  x  x  x  x  —  x  x  o.  o-  x  x  en  — .  os      x  x  — -  x  cr.  oc  cr.  oc  x  x  cr.  oc  cc  oo 


?    !»    Id    ?    M    CO 

O  s  C_c  s  c 

's  -s  -S  "3  5  £ 

r!  O  Or-  O  O 


.CMCOCM.-ieM.-HCMrtCM.-iCM 

CO    CO 

a  a 


■s.~ 


.5.9.5 

2-Ooc  c 


c  c 


:  g  g 
i,a,c 

i  c  c 

IPSPH 


c  o 


c  s  c  c  c 

c  c  c  c  o 

CO  CO  CO  CO  CO 

C  C  C  G  C 


CM  .-i  CO  i-H  (TO  >-<  CO  CN  CO      ,C3i 


c  >ja 

o  o"d  ^"c  2  £  *c  "c  'C  "c  "c  "c  o  'o 


gwsossMa  § 


a  ~ 

c  c 

CO  'S< 

a  g 

c  c 


iiil 

qcpq 


,    CO    tO 


rir 


c  c 


i:  c  o 
pi  pi  c  a.  Pi  « 


OOO        GO 


i-i  CO     CM     ■V     !>• 

X  00      00      00      00 


00         M     N     CO 


Cffih-Tl'      CM 
GO  00  00  00     GO 


^o^  cs  ■f^ooi-icMTroi.eioor-icM  ^-i  -cMt^oc;  j     J       ;       ;       ;       ;       |     j 

••      °  °  oododd      c      d      odd  d  ....'  _J,«rJSrJ^^'^ 

oo^  z  ^^^^     ^     ^^  sz;  o  o  oo   -  ~*     ™      *     ^      *     ZZ 

<*£*         -  «  -.~~~-.^^«.^«.w  ^  ?^A7-iA\     o  oooooooo 

33    p,  d  p.p^aftft^1!^^^^  ^  »333  8  S"  S^  .  cf    S     S"    S     £  £ 

OO      c  o  cooooP-P"     r*     l>   ^    !>  !>■  OOOO    M  awMMMtttxti) 

^^  fl          ^^^^3^3 .  OOCOS  2CD3        3q3~ 

SS      ci  tH  Eh    EhEh    EhEhOOOOOO  O  §§SS   Ph  KKKHWHhS 


H   SB 


a; 

<B 

a 

i 

t. 

- 

X 

a 

r. 

^=J3 

8 

c3 

~. 

a  c3 

- 

fi 

c 

O 

O 

O 

3 

0 

c 

- 

- 

3  ^3 

.- 

2 

- 

d 

g 

i-, 

— 

CO 

Ph 

ft 

- 

ftft 

Z 

0 

fc 

X 

fe 

!Zi 

X 

^ 

ft 

O 

C 

c  0 

^ 

pa 

— 

P3 

- 

« 

PQ 

- 

CO  ■«< 

L-e 

O 

i~ 

00  a> 

- 

71 

10 

t^ 

00 

r. 

s 

—  CM 
CM  CM 

ej 

re 

■e 

OO 

P" 

00 

os 

224 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


spjiBq— pnpoad  leprai 


199J— mdsp  ib^oj, 


199j— q^dgp  no 


•199J— QXXB\d 

ran-rep  9Aoqe  epniinv 


199J— J9A9J 

B9S    Avojgq     gpnjpjv 


•}99J— 
p9^H9U9d  SS9Ulj[0TqX 


•}99j— do;  0)  qjd9Q 


U 


ft  • 


23  o 


X 

si 

So- 
ts 

3  a 
^^ 

—  i  - 

cs  X 

a' a 

qj  a 
9  a 

O  IC 

/-  -r 
00  or 

9  a 
©ifi 

5  ,<- 

ooor 

C  c 

Gas,  864  feet 

Gas,  851  feet 

Gas,  450  feet.    Salt  water, 
474  feet. 

1 

00 

i 

T3 

o 
c 
O 

o 

OiOOO 
O  N  O  lO 

oooo      o 
oooo     o 

■<no 

CO  t>. 

oooo 

o> 

ON 
OS  00 

OOtiOO 

OS  5D  lO  Tt<  O 

oooooooooo 

NOW        O 

§g3    §8 

OCONOOeSOCOiOOON^H         MHiOOaOOCNh-lONaOONOOV 
1  CM  O        (DMNOONOOiOOCSNooCilOlONN 

'OOO  O  O  i-H  O  O  O  i-H  O  O  ^H  ,-H  t-H  O  1-H  ,-H  lO 


ONwiooNNooiNntoffi      t^osioo^iN-^oocoiooor-icHcoc^-ti      .-h 

TflOW^MOiOOOilNfflNNCS         n«NNNH*OON«N001NN         o 
CO  CO  CO  ^_  _|_  Tji  ■*         »o  "*  Tf  ■>*  rji         -^  rjt  CO  Tft  Tt<  tH  CO  M<  ■*  CO  CO  CO  f  CO  CO     l  ■>* 


■WONOOiOKNifllOtOiO'O'        ONO)TOrf(OOONOOHMHl 
MNCO>ONlO*00!O'»i'VN         HfVOJONrtOOOOlOTMOOOfOlO' 

i  oo  oo  •»*<  t  os  as  io  os  os  cs  cs  os   o  o>  oo  oo  o  oo  oo  oo  oo  oo  oo  oo  oo  oo  oo  • 


a  a 


<m'cOt-i<N 

oooo 


ootfl 


tf  : 


J  o  o 


^22!fio°' 


aa 


w  w  03,0  ^  .Q  ©  O^Qp  ^ 
O  O  O  0,0'T3j-  OT3  O'O'O  O  Cd_rt 


!j  1 


-H     05CM     <N     Nh.N     OS     0»H 


o 

£       6 


oo    o*cor^.-i»o-f<co< 


o"  o  d  o'  6  6  d  o 

C/T  crT  c/T  c/T  c/T  c/T  c/T^ 
rO,'^'0'*0''0''rt'3,3 

o  o  0}  op  «  o)  «rQ 


CS      C)tfCJOCJ0Jfl)O  o 

h3  (J^hll-Wl-WH     ^ 


IC 

-JS   iz;   £££ 

'y< 

£££ 

fe 

o 

o 

TohiU,  No. 
C.  Dennis, 

C.  Dennis, 

C.  Dennis, 
C.  Dennis, 
C.  Dennis, 

GO 

B 

£ 
p 

of  cc"  crT 

s  s  s 

QfiP 

3 

I 

o 

ooo 

o 

•3.3.3.3.3.3*3 


bo    bi)  W)  W)  bC  b/D  60  bc.2 


w 

j_j         3     3     ;-j     r-j     r-j     0     3^ 

O 

o 

OO  o 

ooo 

o  OOO 

O 

o 

i— 1     N  CO  t  iO  to  N  00  O) 

8 

si 

s~  N 

COTtilfi 

o   t^ooos 

o 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


225 


1 

— 
— 

1 

0 

c, 

J- 

0 

- 

-; 

- 

1 

0 

Z 

a 
* 

8 

3 

- 
5 

8 

- 

r 

- 
J 

z 

s 

0 

a 

X 

O 

5 

"a 

o 

P 

3 

'3 

X 
X 

8 

3 

05   © 

•2<£ 

00 -H 
— 100 
O5  00 

c/j"  to" 
C3  C3 

oo 

I 

CO 
X 

3 

o 

- 

ue 
t- 

X 

- 
•X 

— 

n 

m 

u 

a 
0 

c^ 

"r 
EC 

8 

0 

- 

■e 

3 
O 
re 

a 
m 

O  ©  O  o  o  o 

t^  S3  o  o  3  o 

*-h  oa  in  co^h 

o  oo 
ooo 

COT*  CO 

□ 
co 

oo 

oo 

COi-H 

o  o 
oo 

OCO 

i 

O 

— 

5 

0 
0 

CO 

CO 
OS 

o 
•a 

oa 

e_j 

s 

OiO> 

ce 

CO       ■ 
OS       • 

§1 

us 

X 

§ 

o-hincs- i^oo^esiaoTfi 

O1O5OS00O3CJ00C3O50000 

•-r 

X 

X 
X 

8 

HNii5ClOHK3HC!NO£MHU5MMO00»f  NMCM/-S:NCL';L»SKH>ifOHNCHVMC«CH 

E;  22  12  S  2  Ei  2  t-  2  L~  —  ~  N  oa  — <  re  os  — >  re  —  —  re  -r  —  o  to  to  re  r-  cs  --  -<  oa  co —  co  — ■  t-  co  re i  ih  co  ^  -w  co  c  oa 

OOOOOOOOOOOOi-iOiOi-hO»Oi-i0^h»--5i-ii-icOi-iC-hOi-iO'-iOOi-I'-i^Oi0^h>-i^hi-i^^hi-i^h 

Oicoo^^ciC^T^c;'^cccTrs^^ot^eo^csic^^^r-^cc^^^c;ueLe^t^c^^Oc;C5CC5i»p?'>»"XC05 

N  H  T  T  C  IN  O  N  O  ^f  »  -h  N  O  H  C  O  >h  ffl  c  c  ft  l:  /  ?)  -  C^  C  M  X  x  /.  c  rex  C  ^  M  r:  N  '/  r:  »  l~  «  C  N 

t  rji  TjiTj«'«jiTTi-«r'<9'Tr'^i  -^"^  co  "3<  _j_  co  ■■»<  _lco  •"cr  co  _£.  co  co  i-i  co  "q<  co^  co-^1  ro-v*  cococo-'J'_j-COcococococotj-co 

oo  105-10 

00      '(MO— '00 
CO      ;CO        (M 

L~CX«KNCNNnO>0 

MNrt       .  <N  CO  CO  CO  <N  O 
00COCO      ;iO>-i        oacot- 

^?4CN 

if)«ac.N 

^  CM  O  O 

-S«  00  o  o> 

t^eOMOWOOOt9«flNOOi010lONO®N»NiHiaO'*MN'*NN®lOgOW'50>(»ONr-i5000'*<CM 
Sfc02N^HOOOHHOO^NiOm.NtOWN«^COgSPNO'*HCO(NNOl«NWNHtO<OMMN'*(5  00  5D 

WKOSOKXSCSKOC.  XX(0C^0000-^000000'<S<0000ce00O00C1000J0C000i00000C02-'r0000CC0000000CC0 

1 

- 

00 

Pi 

p 

c 

- 

1 

0 

i 
1 

M 

pi 

£ 

= 

c 
P3 

p 

f 

c 

B 

c 

IS 

£ 

K 

P 

c 

1 

P4 

c 

p; 

= 

| 

= 

•§ 

1 

0 

1 

pi 

i 
= 

c 
PS 

1 

re 

= 
c 
a 

1 

1 

p 

c 

0 

1 

PS 

i 

£ 

c 

pi 

Pi 

1 

- 
c 

P3 

1 

i 

p 

1 

pi 

= 

c 
p 

1 

P4 

0 

1 

- 

pi 

i 

D 

c 

c 
PC 

— 1 

pj 

V 

p 

X 

c 

PC 

c 

1 

DO 

p 

c 

B 

1 

PI 

i 

c 

P 

c 

V 

P 

1 

ce 

s 

c 

1 

1 
- 

ce 

j 

P 

IE 

c 

pi 

g 

c 

P 

C 

a 
P 

IS 

C 

1 

■s 

p 

'I 

p 

i 

C 

ce 

c 

p 

c 

P 

c 

P 

c 

BE 

P 

1 
- 

i 
c 

p 

c 

2£ 

re 

i 

BE 
P 

1 

- 

;  ^'  cq  i-!  in  r^  rn  ci  ; 

:accccgc  : 

>a.oooooOo    ! 
&  ir.  ir.  ir.  in  xs\  v>  & 

o  s.S.S.S.S.S  S   : 
■3  2  ja  '2  |g  2  jq  2  © 

^  O  O  C   C  O  O  CT3 

t>-  CO      t^      t^ 


SO  OC     —1     NO' 

«o  CO  1 

TJ1   TJ.   ■ 


O     O     O     CO     iO     ■*«     00 

co    co    t^    r~    1--    t- 1»    t^ 


§8    S 


■~ 


CM      •>9<  IO      CO      i-l      .-I 

52  5  55  2    °oo°o    o    6  6    6    6    6    6    6    6  6    6 

co~oT    ot"    aTco*    wT    w  tn  1 


^H  IO  1-H 


._.23ait'32«22a!Mt/3'zlt'3coco 

3  9   S   S  9   S   9'5'5'5'a  g   gg  '3  '3  '3  '3  '3  '3'3  '3 

P3c    P<    P5w    H    Haccc    a    cc3    d    d    d    d    d    dd    d 


OO    O    OO    O    Q^Ha't-aV;    ^    t^^    hS 


1-5      l-S      Hr,       h^)-^      h. 


S5     » 


*  X  £ 

B  £  £ 

%  %  % 

©  ©  03 

Z  ^  £ 


d      o 


.2.2  .2  .2.2  .2  .2.2.2.2  2  .2 
22  2  22  2  22222  2 
oo  o  oo  o  ooooo  o 

■H  CM     CO     tLO     CO     NXOOh 


^    ^    ,*    ^    ^!    ^^    ^ 


oo^^  £  £  ££  ^      p*      II 


o        o 
o        o 


—15  G 


226 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


C/3 

M 

03 

s 

4> 

P3 

Gas,  865  feet 

Gas,  874  feet 

Gas,  860  feet 

Gas.  891  feet 

J 

p 
5 

a 

8 

.a 

spjj'Bq— ;onpojd  ibi^tui 

oooo    • 

(NHN                • 

^99J— md9p  IB^OJ, 

05 

C3> 

•  CJ5      • 

05 

•}99J— IUd9p  no 

CO  t^  CO  CJ5      • 
00000000      • 

0J5 

•6 

a 

o3 

•^99  j— gu^jd 
um:rep  gAoqB  gpnmjy 

»NMCOTPMh.O>NOeON'*t^M'*iONtONl»0>NM(ONrHNCC!C 
rtH(N»WOHCDNM01NONN(NO00©NC0fOl'OHIX)NflMa 
^Hrt^,O^H^r-(O^H^HO--H^-lO^Hr-I^HOOOOrHOO^-lOOO>-lO 

•^99J— I9A8| 

•bos    Avopq    gpn^i^y 

MMI^OfflfflMMNl^ONOlNt^NOlHONtOiOOfOOHNiONO 
CC0OfOTTiCOCO0O'^CO00-^COCO-*0OCOfO-^l-^l-^-*l0O-W|-*lCO^^'^0O'^< 

•;99J— 

pg^Bj^aued  sseu^oiqj, 

tONrr 
CM  CO  CO 

C7>  ■*  CO  O      -co 
TT  (MOO      ;CM 

28£<° 

TfO^H^Ht^rficOiO 
ONi-Hr-li-IOOt-IOOi-l 

•  CM  iO  >C  iC 

•  ^n  CO  <M  ^f 

•199J- &o%  o%  qjdga 

N««30C9'*NOON'*NU5NNtO»OMNHmON<0>OaN<DOO 

CDNlOOi|fl*JNN^'na!COX"-iNNO)iH01NlOfCftMI^ON'*l-C 
OOOOOOOOOOOOOCOJ>OOOOOCOCX'CR0000000500C7:050000CJ300CJ50020CO; 

E 

03 

p) 

c 

01 

P 

2 

c 
35 

c 

c 

c 

i— I 

5 
| 
o 

NCM 

Pi  Pi 

c  c 

c  o 

■o  ;  i- 

«  :  p 

^  :  c 

i>i 

Q   03  £ 
O  £  C 

Scop: 

CN 
P 

c 

i/ 

P 

IE 

c 

pi 

— 

p 

c 
1/ 

c 

p 

c 

p" 

c 
pi 

P 

c 

p 
!£ 

c 

pi 

p 

c 

V 

P 
1 

p; 

c 

.'!    !o-    !!!!!!;!!    ! 

cMcOCMCNlcOrHCMCOlNCO      '.  OOi-HCN 
flrjqgflplpipjflp)     ;plp!p: 
OOOOOOOOOO     .OOO 
(flcnwMcnmtnoiMcn     .  v>  w  w 

5SSSSSS2  9.9  >-  9  9.9 
S  3  2  2  2  S  S  3  |o  3  <s'S  S  S 

OOOOOOOOO  O  >3   OOO 

«p5p2tfp3pJpip3p5P3ccPHp3Pi 

Sur- 
face 
ele- 
va- 
tion— 
feet. 

OiOOOtC 
00  CO  t-  X 



I--        C3S           t^-              C7i        iO        O             CO             OS           i— i        CO        CO 

00        00           OC               GOCJJO               O)               00           C35        CJi        C7> 
■"diTfTT               ^        *        U)               Tfi               -<J<           -*F        ■*»<        •"J" 

"3 
"8 

B 

03 

c 
|Z 
i/ 

4 

P 

c 

c 
!z 
•/ 
e 

a 
P 

C 

c 
V 

I 

P 
C 

c 

•/ 

■p 
p 

a 
P 

C 

I 

'    a 

c 

r 

c 

1 

C 

i- 
c 
|z 

4 

c 

IT 

c 
a 

C 

c 

!z 

a 

"o; 

C 

C 

!z 

v. 

4 

M 

"a 

c 

6 

b        c 

1    * 

03            cr 

C 
C 

5 

c 
c. 

d 

03 
ft 

1 

o 

'8 

o 

1 

03 

c 

C 

c 

5 

c 
- 

S 

c 

C 

c 
c 

2 

c 
P» 

4* 
c 

c 

c 

c 

c 
c 

c 

c 

z 

is 

o 

4* 
o 

o 

o 

c 

2^22  2    £      5        £22        £        £      8    S3    S 

o   . 

CQ 

W 
la 

CM 

• 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


227 


1 

DC 

z 

5 

X 

1 

1 

Q 

IS 

"cc 

p 
a 

c 

-E 

'C 

p 
a. 

' 

"3 

a 

« 

sr 

a 

- 

X 

i 

1 

- 

T3 

9 

CO 

0? 

CD 

XI 

I 

X 

1 

OOO   fe 

S 

ft 

p 

P 

8 

'- 

CN 

CO 

oa 

c 

OS 

g 

.Oi 

CN 

CN 

oo 

XI 

— 

lOiOC 

l>   CO  Tf 

00  OS  O" 

— 

)  iO  CN  -tfi  t—  < 
•  rti  ^H  GO  CO  I  . 

I  ,-h  O  — i  t-h  o  o  .-*  • 


I  O  i-H  ©Oi-H©' 


i  OiOOOOe 


J  CN  iC  CN  CN  rfi  iH  ■*  <*  IO  O        iO  W  iO  H  CO  O)  K)  H 

■-ry.   1'^-    /-'*    /    OiQMXVCStO         COrt^HOSCNCNr^iO 
>©©©.-h©i-<©©.-i  0000050        i-Hi-h©©©©©© 


t^CT>CNCNiOOOcOCOCNt-~C~- 
-^t^©CNiO00^HCOI>-00CN 

cococo-^eoco-^TticocoTti 


COCOCOi— i00r^CN0C»O0000cO©cOcOiO© 

lOMlOHNOOHOO^HfflttOHIIJO^ 


CN  i-H  (M  CNCN  i 


'  00  IO  CO  Ttl        .IOH 
■i-li-HCNCN       •         i-H 


•OOOCOr-loOiOOO 


/ :  '  -  x.  :■-  c  — i  ;c  — <  s  i 


i  CO  CO  CO  CN  CO 


i  ©  oo  oo  oo  oo  i 


•  o  >o  oo  io  r- 


CS.O 
J3  ° 


lCNCOr-H  CN  CO 


>>.p;.p! 

03,0.0. 

£  o  o 


S  Pi 

~  c 
/.  ./- 

.a  >,S.S 

,Q  03,0.0 

•    o  o 


CO  i-H 

h  h 

o  o  o  <_>   oo  .oooo^OO 
CO  CO  CO  CO    coco  .  co  co  co  co  !>  co  c« 

rt  PI  pi  pi      pid:plp|pl  q_o  pi  d 


;  CN  CO  1-4  CN  rH  CN  H  CO 


.NmrHCTHlNrtKIHrHmTprtCMm        ,  .  1— I  CO  T-H  CO        ,  H  CN 

pipipipispirtpipipipipipipipi  :  :  pi  pi  pi  pi  :pipi 

.OOOOOOOOOOOOOOO  ,  .OOOO  .OO 

3  3  3  3  3  2  io  IS  3  3  3  3  3  3  3  3  ©  cs  3  3 

ooooooooooooooq  tJ  £  o  q 


>3   O  O  O  O  O  O         O  CO  O  O  O  Ofj  O  Of  OOOOOOOOOOOOOO  Of         hoc 


J2 - 


-d  O  o 


t^    co    >o      r- 


£   s 


CO 

c 

c 

C 

if 

C 

CC 

c 

CN 

c 

CO 

c 

OC 

c 

c 

c 

*c 

CC 

t> 

CO 

IO 

£ 

& 

£ 

fe 

^ 

» 

a 

55 

fc 

!Z! 

PI 

PI 

PI 

PI 

q 

p: 

S 

PI 

PI 

PI 

o 

o 

o 

o 

o 

o 

o 

o 

o 

o 

Cj 

cy 

.2 

^H 

aj 

^   ^ 


^   ^ 


o    o    o 

fc  ^  ^ 


O    O    O      O      O    O 


O     CO 


-3  -9  -9 

TO       to       OT  C^ 

s  s  s   a 


^        c3     c^        c3 

CO  CO        CO  CO 

-9     -9  9  '  -^ 


s   s 


^    PI 

C3      O 


^a  ^  ^ 
o  o  o 


rr  iO 


228 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


spxreq — lonpoad  i^prai 


•188J-  ifldep  xev>& 


•}88j— tftdep  no 


a 

o 
D 
I 

a. 


I 

8 

o 

•a 

is 

O 


•^881— ^U^ld 

ran^ep  eAoqB  spn^i^v 


•^88J— I8A8I 
•B8S     MO\QCL      8pn;i;xV 


•;88J— 

p8^j;8uad  sssn^oiqjj 


•^88J— do;  0}  md8Q[ 


oo +j 

"S  "o 
£o 

±i  co" 
02  0 


00  00  Ci  CM 


OOOM 


OP 


O02 


03  fl 

Is  to 

S  (=1 

02 


I— 1  CO  <— 1  -^  05  CO  05 
HNtOCO  QC*C5  CT> 
T-f  0000005 

O  OO  i-l  05  CO  l>  CO 
CM  t~-  00  CO  CO  CM  f 

T-H05005000 

COO»-IOOCM0005COCO 
COlOtOONOllOOO'* 
OOOrHOOOOO 

COt-rtMrtN 
rHt^O>K3COTI< 
rHOOOOO 

Ol  ■*  O  CO  H  ■*  rH 
QONCOCOHOO 

CO  -Ct<  -^1  Tt>  Tfl  •<»<  »0 

0<N05rH-V«N 

00  CM  ^H  CO  CO  t^  lO 
CO  iO  Tf  lO  Tfi  T}<  T}1 

NOONWNiHNN 
^i  ^j*  ^  CO  ^  ■*}*  ^  ^  ^ 

-CP  CO  05  l^  05  CO 
00CMO^O>O 

M  >c"  Tti  ■*  ■*  V 

o  >o  iO  iO  CO     •  o 
riri              CM      -CO 

co    'H«ico>o> 

•  CMrHrtCMCM 

8°S88  |S  :S  : 

2  ;S  JSE 

r-  <N  iO  CM  t^  CM  CM 

lOOOMt^tON 
00  00  05  05  00  00  05 

845 
994 
895 
1,007 
900 
939 
927 

COCOCMCMOOt^cOCOCO 

00CM^HCOO5t^^O5CO 
00  050500000005  00O5 

cCOOOOCMCO 
"OO5  00H00N 
00  00  00O5  00O5 

:  a 


|CM  CMcp. 

a  a  a  pj 
o  o  o  o 

>3  O  O  O  OTJ  o 

^psphPhPh  :« 


CO  i-H  CO  CM  CO 


>>3 
03,0 
H  O 

02  « 


asasa 


O  O 


O  O' 

tftf 


hpjNhNhco 

a  a  a  a  a  a  a 

o  o  o  o  o  o  o 

to  co  co  co  co  co  co 

.9.3.9.9.5.9.9 

o  o  o  o  o  o  o 

P5  P5  Pi  Ph  tf  tf  Ph 


co  w 

«3 

o  o 


rH  CM  .-I  CO  CM  CO 

a  a  a  a  a  a 

o  o  o  o  o  o 

co  to  co  co  co  co 

a  a  a  a  a  a 


p?rtp5p3P5« 


CO    CO    o       >o       CO 


s  n 


c 

"* 

CM 

CO 

"»<  t—  CO  00 

6      6  6  6  6 

53     53  ^^2 

pq     po  pqpqpq 


.53  o 

Oj  53 

53  .S  - 

So  « 


o    o 

£  53 


53    6    d 

^  53   ^ 


o      o      o 
53     53     53 


I'll 

K    Eh    Eh 


o      o 
H     Ei 


,a    ,a 

o      o 
Eh      Eh 


CO       CO 
CD       CD 

2  2  2  2  2  <1  2  S  95 
a  a  aaa  0^  o  o  o 
o    o  OOP    So  M    M  W 

•V        i«     CO  C-  00        OO     i-i        CM     CO 


£      CD      CD         CD         CD  CDCDCD 

gaaaa  aaa 

«3aaa  =333 

a  pq  pq     pq     pq  po     pq     pq 


SZ 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


229 


c 

s 

$ 

s- 
- 

a 

r 

(- 
a. 

r 

is 

"r 
X 

- 
p 
- 

c 
c 

o 

CM 

© 

"3 
aa 

(- 
a 

0 

ft 

0 
X 

— 

c 
c 

a 

0 

y 

c 
c 

I 

7 

c 

c 

CO  >>>.. 

r. 
M 

S3 

3S 

t~~      © 

©         © 

CM 

© 

CN 
OS 

so 

CO 

5 

05 

O  t- 
to  iO 

0105 

Oi 
X 

OS 

1- 

OJ 

CN  © 

©00 

MOO 

0O  CO  — < 

oo©  © 

io  rt<  oo  co      nmohm 

O  -r  O  CO        «HfflOH 
©  ©  ©  ©        00O>XOiO) 

, 

OS 

DCOMSJHNTftNfMNCf'H         lO  CN   Sj  CO  -H  T  CN         n  CO  'O  *  N  N  t  h-  iO  t^  t~  X  CO  -r  '■-  CS  CXj  O  CO 

KraiOOOTTOlOffltOONWtOH         OS  SO  OS  00  f fN         LlfHOiNNTIHOOHMOOOHOOinOJNO) 

TfOOOOOOOOOOOOO       OOOOOOO        ©©.^©OOOi-i^Oi-ir-iOi-i©©©,-!© 

NOCC 

NONHffllOO<DtDCOOt>OONai         iO  CO  CN  -*i  ©  CO  CO         NNiONWOCOMl'-jKCCIMNOIOhNON 

iHrt'*HiOO'*C<5COaN!DCOC/)         OMOh««3N         tjnooOOMtMlO^OMtOfflHXHTl-OOCO 

Tji  ^  ^i  ^  ^t  ^1  ^Ji  ^i  rf  M*  "«CH  ^  ^ct<         Tt<  ^  ^  "^  ^  ^f  ^         ^  ^f1  CO  ^CH  ^  ^1  ^CH  CO  CO  "^  CO  CO  ^  CO  ^*  ^  ^  CO  ^f1 

t^  OS  i—l 

coco  ■* 

MNMOHNOltONMNO 
eqHNNNHC<5C<l(NrtiNHN 

MONhNCON      oo  ©  >o  i-h  >— i  co  ©  Tf<  ©  to  >o  co  ©  io  © 

NhNMhNh             CO        HM        .-1,-ii-c        i-H        »-Hi-HCN 

sa 

1^ 

CM 

t-oo 

1-H  CO 

CO -H  00  CO -CH  IO  CO  OS  ^H  © -H  CN  CO  IO         NtONrHlOOlO         M^tDWWNOOCOOCt^CDrtNtDNNCBH 
00«rt00M00NOHt0Ol«OO         00 -H  OO  O  rt  CO  lO         T|<lON0)WC0®'0'Ot»lOMH00rt'*O00rt 
•^  CO  O  00  ©  00  ©  ©  ©  ©  ©  ©  ©  ©        00  ©  00  ©  ©  ©  ©       ©  ©  OO  00  ©  ©  ©  00  ©  ©  CO  00  a>  00  ©  ©  ©  00  © 

OS 

IfllOOS 

toooo 
ooocos 

1 

X 

CN 

§ 
1 

CO 

§ 

F 

1 

<M 

£ 

D 

c 

pa 

r 

g 

c 

CM 

p 

c 

1 

£ 

c 
P3 

F 

c 

c 
P3 

i 

c 

g 

c 

c 

i 

1 

pa 

CN 

= 

c 

! 

c 
P5 

g 

c 

g 

c 

CN 

£ 

c 

a 

pa 

co 

i 

c 

pa 

i 
g 

c 

P3 

5 

0 

c 
P3 

i 

c 

g 

c 

PS 

p 

p 

c 

g 

'1 

€ 

5 

0 

1 

pa 

« 

p 

c 

s 

c 

pa 

CO 

pi 
c 

I 

c 

p 

c 

D 

2 

c 

i 
I 

-i 

I 

c 

1 

2 

c 

? 

c 

> 

F 

c 

ir 
F 

12 

c 

F 

c 

B 

c 

p 

PI 

c 
w 

F 

2 

c 

F 

c 

0 

2 

c 

pa 

E 

c 

g 

2 

c 

CN 

PI 

c 
E 

c 

CO 

i 
f 

2 

c 

pa 

c 

1 

2 

c 

CC 

F 

c 

f" 

c 

pa 

F 

c 

1 

c 

p 

Fl 

c 

fI 

2 

c 

r— 

i 

F 

c 

c 

F 

2 

c 

pa 

c 
2 

c 

pa 

^h'cN  CO 

o  o  o 

co  m  w 

9  2  S 

o  o  o 

papapH 

n    co    n 


CO  CM  00  iO  t--  CO  < 

r^        oo  t^  oo  coco  ( 


§    g 


fiOMON 


CN        CO     00     N 

6      odd 
55    55  fc  £ 


"!^d 

odd  d°  ojz; 

o  o"  o~  o"^"^f  fc 
"es  ri  "S  "cs  '£  '£  £ 
Oh  Pm  Pm  Pm  fe  fe  5S 


rt  CN  ^H 

odd 

55  ^5  55 

i/T  »r  »r 

^  ^  ^ 

.2  .2  .2 

£  w  w 


-i= 


cd  co  55  o  cT  -  - 

ot  co        co  co  m  c3  rj  .rt.PT 

.2  .2      .2  .2  §     .     .0302 

M       W    W  M  hW52h>-; 


55    55  55 


Oh      CQ    PP    P3      PQ      PQ 


#<% 
%*    . 

22  5 

o  ct>  as  cu  ^^..rti 
fl  PI  a  flts"c3i? 

SgHSggo 

pa  cq  oq  m  fh  fh  5i 


o    o 

fc     f»H 


rt  pi  pi  „   , 
1  £  £  £  PI  « 

S    o    ^-'o'H'cl'elS'aa 
^  jz;  ^M53P^m 

t~-     CO     CS  O  ^H  CN  CO  -3< 


230 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


s 

o 
o 


</5 

2 
© 

c 
c 

ft 

c 

c 

c 

3 

c 

c 

c 

rz 

:    -c 
:     c 

c. 
a 

•       c 

:    z 

c 

c 

c 

•spxiBq— }onpcud  pBprai 

•laaj— q^dap  iinox 

•GO 
■  iO 

•as 

- 

CO 

as 

-<       'CM 

as    •  as 

•  j88j— mdap  no 

1 

CO 

•^88J — 9WB\d 

raniyep  aAoq'B  8pn;p-[y 

i— l  ■— l  o 

as  i^  co  -h 

(NOOOiO 

-HrHOO 

M  ■~   1  -  — i  ~   CO  CO  O 
i-IOOt-IOOi-HH 

■<CKCOCN 

COOGO 

i-H   ^H   O 

■%Q9l — \QAQ\ 

■B8S    MO]9q    8pn;i;iv 

F^oscn 

CO  CO  -f 

>-h  co  ■*  as 
t^  as  -h  ■* 
CO  co  -w 

y_  r-  go  cn  cn  -h  as  rH 

t-OCNGOOCOCOOS 
CO  ^P  ^cfi  CO  ^  ^  CO  CO 

co^f  GO 

coos^h 

CO  CO  t»» 

•198J— 

pa^BJieuad  ssaujprqx 

CN 

COT  rHCO 

H«WH 

-cr't^^O-fcO-HCO 
r-li-l-^IMi-ICNi-lTf 

Tji   Tf»  CO 

•^88j— do^  oj  mdaa; 

t^  t^OS 

CO  GO  i-H 

GO  GO  OS 

•f  CO  t^  CN 

CDOOOTti 

go  coos  as 

GO  t-  X'  CO  CO'  lO  OS  -H 

NooNONmoo 
GoososGoasasGOGO 

CNO* 
GO  00  OS 

9 

2 

P 

c 

■r 
P 

c 

CN 

P 

0 
P 

2 

c 

« 
p 
c 

P 

2 

c 

2: 

p 

c 
■f 

p 

2 
c 

= 
o 
co 

lo* 

o 

P5 

Pi  pj 

s  s 

32 

c  c 

i 
c 
r 
P 

'2 
c 

p 

c 

V 

p 
2 
c 
PS 

P 

c 

V 

e 

c 

pd 

c 

V 

2 

- 
c 
pc. 

CM 

P 

C 
K 
P 

2 
c 
Pi 

^- 

P 
C 

I 

- 

c 
pd 

o 

CO 

| 

2' 
c 

g 

s 

D 
O 
4 

rH  CN  CO* 

o  o  o 

CO    CO    CO 

q  q  pi 

■s'-s'-s 

o  o  o 

PhPhPh 

-3  o  05  c3  q  ,<u 

co.2  »  ^.2.2 

CD        iO 

OS        O* 

CO        t-  CO        O               -r            O            CO        CN         ifj        iO        CO 

asasoo          as        as        ososososos 

CO 

as 

"3 

© 

E 

03 

CN 
C 

(- 

a 
q 
c 
b 
bj 

C5 

c 

"  g 

- 
p 

CO 

c 

a 

§ 

bi 
bi 

OS 

CO 
C 
J? 

3              bi 

03 
Ph 

IT. 

c 

CB 
3       b/ 

-z 

<& 

Pm 

C 
1 

A 
I 

2 

o 

p 

CO 

c 
125 

V 
II 

CN 

c 

2 

w 

•* 
C 
fc 

0 

tu 

03 
Ph 

c 

a 
bi 

03 

Ph 

o 

/ 

« 
bi 

'S 

Ph 

CO 

c 

I 
1 

Ph 

c 

.2 

HH 

2 
o 
o 

'o 
"3 

05 

2 

03 

1 

1 
W 

g\ 
11 

05  CO 

co 

c 

r3 

■   -8 

« 

en 

q 
3 

03 

w 

q  © 
S-3 

3  p2 

©CO 
CO 

co     '  co 

q   :  q 
3  :3 

£      •  £ 

03        03 

W  :W 

co"    !  c/T 

q  cu  q  cd 

©co  ©co 

CO        CO 

a 

c 
- 

03 

W 
a 
oi 

Ph 

oi 

& 

s 

03 

Ph 

:  m  :»3  :«a  :°8 

'     co     'co     'co     'co 

:   S   :  S  :  B   '■  B 
:  3  :3  :3  :3 
co  ^  ;  *  :  *  :  * 

"«      03      ,  03      ,03      ,  03 

%  M   :M   ;M   ;M 
&        •      •      • 
•o    .  :  „  :  ^  :  ^ 

^7    q  oJ  q  <u  q  ©'  Ph^o. 

^       Ph-S   p^-Ss   pq^i   ft-S 
g      05  CO  _g  CO  ©  CO   »  CO 
Pm     CO       CO       CO       CO 

^2 

? 
id 
W 

8 

S 

Ph 

&6 

•*#                CO      t-                   GO         OS         O         ■— I                CN             CO      f         iO         CQ,        t—                GO 
^                ,-H      ,-1                   ,_,         _         CN         CN                CN             CN      CN         CN         CN        CN                CN 

q 

o     . 
33  o 

en 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


231 


0*0 


>c 10  co  g  io  00  m 


c3  c3  c3  O  03  03  03 

cooizooo 


00 
in  © 

— 1  <N 


ss; 


-HMOlONNrtCDHN 
t-*t-HOOt-H©.-HOt-HO 


NintOOHN 

o  <n  cc  to  y  1  - 

^0t-Ht^--*,-IO.-H.-I©.-H,-H,-I,-I,-hOt-H,-,Ot-H,-hO.-Ht-H,-<0000 


O  tO  W  tO  O)  O  (O  ifl  10  t)( 

gggo-sogsgg 


OVN'9'HO'^iOlOtO 
-MHNUJfllOOOM 


1  C5  CO  iO  rrj 


'irocococo^cooo^cocoeococo^coco-vfOco-^cococcicO'^TPTr 


T-H  T-lCO 


■WrHNNOCBNiO 
1— I  1— It- IHNHr- It— (I 


:3S5 


CO  00  I~~  00  CO 


ooiot^-r^iMr^O't'iO'*1 

NtDOJNNHOOINNH 


X   -f  ~)  -v  —■  ci  : 


1  -  *  1*  "O  c  c 
1  CM  CO  CO  t~  -V  05    - 
S    /     /    /    S     f.    f    X  X 


.       cocoioico^t^-^-t^cocNiTrico 

00000500000005050105 


O  00  Tf  O  00  CO 

(NrtOrtMN.,. 

O5O5O5O5O5000000 


ON00 


—I       .  C-Q  CO  <N  CO  OJ  CO  (N  CO 


.00,0,0.0,0.0,0,0,0 

0"0  00000000 


hNhNhINMhNP5h 

opiopipipipipipipipi 


(N  rH  ,-H  <N  H  <N  CO I  7-1  <N I  ft  CO  CO  <N 

.OOOOOOOOOOO 

:S.BB.BB%S5SBB  ■ 

1 2  2  2  2  2  2  2  2  2  2  2 ,°°  2  2  2  2  2  2  2  2  2  2  2  2  2  2  2  £ 

'OOOOOOOOOO  O'O'O^  000000'->'^'-'~ 


000000000000000 

o  2  2  p  2  2  .0  2  2  2  2  22^j- 

JOOOOOOOOOOOOOO  OT3 


CO      ,CN 

d   :  d 


JDO^OX!  C3  0  O  O  r> 

co  cd  o  s-  cdflo 


00        00     001 


CO     10     <N 


-r  <M 

05 

^ 

CO 

CO 

ZZ 

*H 

•* 

CO 

<M 

O  O 

O 

O 

0 

O 

ZZ 

fc 

2 

z 

Z 

O   O 

Z 

Z 

z 

z 

Sfl 

a 

g 

_d~ 

_Pj 

PI   Pi 

_g 

rf 

pj 

d 

I*!* 

* 

-= 

l* 

(* 

js  £ 

J_, 

o> 

» 

<» 

(B 

ZZ 

Z 

z 

Z 

Z 

^H 

^ 

s 

£ 

§ 

o  o 
ZZ 


000 

z  z  z 


CO  00       OS  T-H  1>  t— I  CO  00  T- It- IH 

6      6    666060600 

Z     Z  ZZZZZZZZZ   00'  r~'  co' 


■y    t/t 

I/) 

.3 

2 

■f. 

23 

2 

W3 

ITi    Ifl     W    IT.     tTl    KTi    in    IT:    W 

0    0 

0 

P!  Pi 

Pi 

q 

3 

Pi 

PI 

d 

d 

CflCfic<c4CSfl 

z  z 

V 

Pi  Pi 

= 

q 

pi 

a 

Pi 

a 

a 

CfifiCflflCficl 

<B 

a> 

© 

CO 

0}OO<DG}Q}Q}C}Q} 

00 

- 

0 

0 

p 

Q 

0 

0 

fiOOOOQOOO 

0    0 

0 

2SS. 


232 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siaxreq— jonpoid  vbtiiui 


•;88j— mdtep  i^oj, 


•}99j— q^dgp  no 


MONiQOhh 
CT>  Ol  00  O  O  O  O 


^ 


8 

O 

•a 

o 

8 

C2 


•^89  j— eireid 
rar^Bp  9Aoqe  apn^iv 


^H  O  ^H  O  T-l  1-H  O  1 


1  o  ,-h  o  c  /  or  /-OOKJOH 
IO.-HO.-IOOOOO.-IOO--H 


0000000000 


•}99J— I8A9T 

B9S    j&ojgq    gpn^jy 


•199J— 

p9^j;9U9d  ssgujpiqj, 


•;99j— do^  0%  qidgci 


i*00OOMOlCNU3l(5O00  00OOOOOO010!HHONn0)HTf 
iOO)N90N01NrthO!010)01»COW(NNOOOW01HfflOiQN 
'0000000000000000000000000000005000000505000000500 


00000000000000 


.0,0 

o  o 


9 

■§■§■§ 


co 

pi  pi  p) 
000 


HMH 

S3  fl  S3 

000 


aaassaa 


lOOOOOOOOO'O'O^OOO'O^O'rt'd'O^OOOO 


0,0,0 

000 


g  06  <s  p)"5 
02 .2  «  >.2^S 


s§  3 


00     CO 
!>•      OO 


t—     rt<        O     "tf>  CO  t^  UO     O        10     O 
GO     00       00     CO  00 t^-  00     00       00    00 


o    o 


O  00     O        10     CO     CM 


£  fc 


0000 


o     o  o    „   „ 


0000 
£  fc  £  5? 


Ph      Pm      Pw    P-iPh    P-i 


03  03  a?  S  S  FJ 

o  0000  o 

'£  'S'C^I^  ,0 

p,  PhCUHH  Eh 


ass 

000 

.0,0,0 

&     fH      &H 


o 

03 

i 

ft-; 

C3  O 


jo 

r 


a 

a 

? 

a 

03 

ffi 

OJ 

a 

? 

0 

B 

O: 

PS 

1. 

a 

0. 

s- 
0 

F 

a 

P 

S 
P 

pL,  PhPhP3W  pq     pa  pq  pq   pq 

-H     (M  CO  i-h  CM     CO        1<     K5     (O     t» 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


233 


a 
a 

— 

c 

"r 
DC 

1 

c 

Is 

X 

Gas,  912  feet 

Gas,  920  feet 

Gas,  905  feet 

Gas,  907  feet 

Gas,  912  feet 

Gas,  975  feet 

Gas,  893  feet 

Gas,  906  feet 

c 

L 

c 

(1     ' 

0    • 

0    • 
<o    • 

S-   O   C 

55  : 

c 

c 

00000000 

NOiOifWWOO 
NrH                     P1C<J 

10 

0 

MS 

iC 

00c 

F*> 

t-l 

n 

X 
OS 

00  C5 

as  as 

o 
o 

1^ 

0 

OS 

s 

c 

I 

CO  C5 
C5  05 
05  05 

5 

CO  t- 

05  05 

CO 

as 

1- 

lOOOOWOOiOO 
O5O5O5O5O5O500O5 

I- 

OtSNM^NiOfJi^HTnOHioaiOOltOHlNOTft-OCcat-NSXONiCCONiOH 
MO^HiCTIicOOOiONMlO'J'OlCONNOlXOOCcoOHOXCrtMfflONKJNHMO 
©©OOOOOOOOOOOOOOOlOOr-ir-ir-iOr-ii-ir-iOOi-iOOr-iOOOT-iOO 

OCOr^OOOrH© 

ONOONOMiOCai'OJOiflOHCHOHfl'OOOOfflnOHHMMtNOKWNMOOl 
eO*lOOCNiO©rtTt«NrtM.OOOMNOHC»OC;--C.OCSHCOXHMON^NOCCq* 

OXCDOlCONOlO 
tDHNOCONOOC 

rrooio 

TPt>iOO(NinOiNMiOOOM 

r-l  r-l  IM  rH  r-l  (N  r-l  r-l  l-l  t-H           r-l 

,_,  ,_,<?$,_<,_,  r~(  r-l         rH  rH         H* 

ifllOH^HMCM 
MNrHrt«rtPiS 

N^^t^TjuDt^Nl.'JOOrtMiOHNOCMHrtOOHNr'.  -XOrCSNCCH^COlClWS 
e»OJC505C303050505a5a5a505a50505O0505a505a5C5C>Ca000O5050GC5O5a5050505000sa5 

OIWMCOOWO 
(ONOOHNOOOOl 
050000305050501 

I 

c 

'1 

pe" 

c 

p 

i 

P 

p 

c 

c/ 

p 

'1 

pi 

-r 

p 

c 

p 

X 

c 

pe 

i 

z 

p 

X 

c 

pe 

p 
p 

c 

y 

p 

X 

c 
pe 

I 

V 

p 

— 

I 

V 

X 

c 

p 

c 

c 

FJ 

X 

c 

p 

c 

p 

c 

p 
~z 

p 

I- 

i 

1 

p 

P» 

i 

- 
c 

p 

p 

p 

c 
y 

p 

1 

p 

I- 

F 

c 

E 

X 

c 

p 

J* 

p 

c 

I 

c 

p 

c 

"C 

> 

I 

-7 

F 

z 

.  p 

-: 
c 

p 

c 

c 

c 

c 
- 

p 

C 
cc 

p 

1 

p 

1- 

p 

c 

y 

p 

X 

c 

p 

c 

c 
- 

p 

c 

c 
a 

p 

1 

p 

i 

y 

p 

1 

p 

T- 

p 

c 

p 

X 

c 

p 

0 

i 

p 

'1 

p 

f 

c 
y 

p 
IE 

c 

p 

— 

p 

c 

X 

c 

p 

fr5 

i 

p 

"1 

pe 

F 

c 

<y 

p 

X 

c 

p 

p 

c 

p 

p 

F 

c 

1 

X 

c 

p 

p 

c 

c/ 

p 

X 

c 

p 

z 

p 

1 

p 

f 

c 
p 

X 

c 

- 

c 

1 

F 

c 
p 

1 

p 

c 

p 

c 
-y 

p 

'1 

p 

:■ 

F 

c 

c/ 

p 

X 

c 

p 

If- 

:i 

\l 

"C  C 

:pe 

C' 

i 

ry 

p 

X 

c 

p 

t-      a    n 


05     OttDOONOiON 

O      r^OOOrHOOO 

10    113  o  o  w  m  10 10  10 


10     10     10  10  10  T  >«• 


•*.      t^ 


CO      r^  CM 


o     0 


6  o 

1 1 1 1 1 

^  ,q       o     in       id 

EH  Eh 


53   55     Z 


tjI  ^  id  cd  i>  06  c<i  co 

6    6  0  0  6  0  6  d  6  ,_; 

55   55  55  55  55  55  55  55  £  6 

c3    c/T  oT  t/T  i/T  aT  wT  en  ot"  ^; 

&  KKKWWWKM  § 


pj  S 


lis 


000 
55^55 


o  c 

^55 


pqpqpq 


o      c 

s-,        I* 

pq     pq 


d     z     Z    Z 

W     ffi     h  fe 


PP 

u> 

53  .2.2.2  2.2  °  9  ° 

&  33x1x1x1x13x1 

_fa   OOOOOOCO     Pt5 

uO-  !ON«050hNco 


>>>>>>>.>> 


00000 


rC  ©  05  «  CP  a> 

■g  ^^^^^ 

O  C3  C3  c3  c3  c3 

55  Pm  Plh  Ph  Pm  Ph 


t^  00  05  O 


234 


OIL  FIELDS  OF  CTJAWFORD  AND  LAWKENCE  COUNTIES,    [bull.  no.  22 


•spjjBq— jonpojd  fepiui 


•}9aj— mdap  ib^oi 


•19aj— tndap  uo 


ninjBp  eAoqe  aptniijy 


•J88J— PA8X 


•188J— 

pajejiauad  ssaujpiqx 


•;99j— do  j  01  mdaQ 


i,  ©  i   i    I  .j 

3  o  ©  a  p-£ 

r£^    ©    ^.2<2 


§z 


£5 

31  3". 


p  © 
o» 
o  — , 

8  SB 

o     « 

O   r-/"- 

O  S3 
co"0 


CN  X 

■X  —I 

3!  X 


*3S 
ii  eg  aT 


3^ 


^00  £ 


COOcO 


zo 


OHOOOlOlOHH' 


I  -  •-£    —    rt  ,-   ^  rt  IN  rt  ! 

t  to  io  ic  tt  lo  a  rt  co  io ' 

lOl-H©r-lCO^HOl-t©^H< 


CN         •         '^^H 


OOOONffltOiQ' 


a  d 
o  o 

SS 

S'Jo 
o  o 

Pi  Pi 


-h  CN 


o  o  o 

Pi  Pi  Pi 


^rS-2' 


I'd  c 


p  p  p  pi  pi 
o  o  o  o  o 

O  O  O  O  0£  o  o  o 

pi  03  pi  pi  pi  co  Pi  Pi  Pi 


CO>-i  CN 

P  P  P 
o  o  o 

x  ai  t/i 

P  P  S3 


382 


QO  »l-*X0000 


CO  .-<  CM  CO  CN  CO 


Clflflflfl 

o  o  o  o  o 

M    [»    to    M    01 

p  gs  g  g 
3  22  3 ',3 

o  o  o  o  o 

pi  pi  pi  pi  Pi 


p  PI 

o  o 

as 
II 

PSCS 


r-       co    ©■ 


§  §  § 


cm' 

CO 

o 

o 

o 

o 

c 

Z 

fc 

fe 

£ 

z 

'H 

P 
© 

d 

© 

p 

© 

p 
© 

P    to 
© 

CN 

If 

1-1          — 

1^ 

1—1 

B 

-H                   CO 

s    s 
s    e 


s   p"  p~p~  g 

o     3     ci  ci     3 

g    £    ££    £ 


O     CO     COCO     CO 


a  g  d'Spf  sT 

2  2    2  ^"3  53 

£  S   £3^  4 

B  3  .&«>  B  I 

CO  CO    co-<S  S 


o    o    o  o    o 


P  S3 

"SCO  *      >>        >*» 
o   73     ,2     2       2 


O     O   ^PhPh 


lO     i-H     <N  CO'    rf 


23  C 

©^ 
co 


."Ms? 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


235 


; 

c 

r 

• 

s 

£ 

7 

: 

CD 

s 

'3 
0? 

7 

. 

OS 

-O-w, 

• 

g 

>d« 

J. 

aft 

_i 

. 

V* 

1  8 

«£«£ 

o§ 

o 

s* 

ex 

CD 
CD 

s 

"e3 

S28 

60 

C3 

x£ 

a 

0 

is 

£ 

5    ~p 

±5        co  o: 
"3        03  c/- 

•-00  00 

ZO 

O 

'Cui 

'Z 

DD 

-x 

cc 

o 

& 

CCC 

o 

CO 

to 

>. 

>> 

c 

tt 

CO 

g 

ie 

OC 

X  T  C<" 

n 

p 

1  - 

[ , 

X 

<': 

CO 

X 

t- 

I- 

y 

Sc 

Sc 

_ 

_ 

OS 

a- 

OS 

a 

a 

a- 

a 

a> 

00' 

to 

ffi 

SSS 

X 

B 

B 

8 

00 

00 

*CT 

CD        ■ 

35 

a 

OC 

OC 

oc 

OC 

X 

XX 

NWH 

■  M  r-  ^h  t—  CM  Tr 

~r  i> 

N-HOt 

cc 

uO 

T 

fxentcK 
"*  ^  -1 E= '-"  S  £ 

c 

t^  CN  I> 

•  CO  t^  CO  r—  IO  CO 

CO  iC 

to 

CO  « 

--. 

CO  CO  -1" 

•  t--  CO  0>  CO  00  co 

•  CO  CN  CO  CN  -r  CO 

X  CT>  O  CO 

^r  lc 

>c 

COCNtN(DOI> 
lO  !.■:  X  N  T  N  Tf 

LO 

tc 

t^ 

lO 

TT  CO  LO 

CO  CO  '•J' 

■  CO  ■*  CO  -*P  CO  -& 

co-» 

Tfl    CO   TJ<    ■«*> 

rf 

CO 

co 

CO  CO  CO  Tf  CO  TP  TT 

M 

CO  CO  CO 

iO 

~ 

00  CO  00 

r 

8co 

CO  X  iO      • 
Ci  t~  CO       • 

HT 

o 

O  to 

— 

OCOOOCNUO^ 

in 

X 

©tea 

•^      i—i 

'Oeotooo 

'MXCC/C    r 

•  OC  00  00  00  00  00 

•«J<   lO  — <  t^ 

8 

s 

S3S 

00  Oi 

B 

R 

R 

3  ^r  O 
00  00  OS 

0CO! 

OlOOiOi 

— 

02 

00 

oc 

OC 

00  X  00  0C'  OC'  00  CT> 

00 

OC 

OC 

X  00  00 

Bi 

K 

!cn 

CO 

p 

ro 

co 

CO 

CO 

CO 

CO 

CN 

co 

71 

CO 

CN 

afii: 

:  p  rt  a  s  p  p 

fl  p 

rt 

P  P 

p 

PI  c 

£ 

PI  G  P  P  P 

p 

g 

c 

o  o  c 

.  o  o  o  o  o  o 

o  c 

o 

o  c 

o 

o  c 

c 

o  o  o  c  c 

c 

c 

- 

pISp 

■    CO    CO    CO    CO    CO    CO 

.  p  p  a  fi  a  d 

co  cr 

P   P 

B 

CO    CO 

PI  PI 

3 

co  co 
PI  P 

CO 

Pi 

CO    CO    CO    CO    CO 

p  p  p  P  P 

CO 

p 

p 

co 

p 

-0,C,C 

..O.O.aio.Ciia 

,Q,C 

,Q 

£:& 

£2 

&£i 

X 

O   ©,Q  ,0,0.©  £2 

o  c  c 

•  o  o  o  o  o  o 

o  c 

o 

o  o 

C 

o  c 

c 

■Cd  o  o  o  o  c 

C 

c 

- 

'U  '0  ^J 

« 

2 

tt 

:ps 

pi 

tf 

- 

rt 

ti 

« 

pi 

Pi 

« 

« 

tf 

pi 

M 

« 

x 

- 

~ 

« 

^ 

« 

« 

rt 

s  s 


5   d 


o      o 


^     ^ 


^      £ 


2     £ 


o      o 


z   z   ^   fc   ^ 


»   z   z   £ 


22 


tf    tf       PJ    PJ 


tf     pi     p5     tf     Pi 


cj    Pi 


Pi    Pi<;«i 


P  :p 

o  io 
So  go 

2   "C  S'C  PI 

P      g  «  S   CD 

s  IhIs 


i. 

'•   ft 

ft 

Ift 

o 

•  o 

o 

CD 

•  CD 

CD 

•  > 

•   > 

CD 

■   CD 

CD 

- 

:p 

- 

:p 

^ 

:^j 

•3 

:^j 

o  :    o  :o  :o  io 


o  :o  . 
§SgS 


_   ;o  :o  :o 

go  go  go 


-   io  io  . 

go  go  go  go  go 


■g  P'C  G-r< 

5   CD    £   « 


O    —    CJ  _,    ^ 

ogo     go 


<    <        <d    <1 


SS 


Ills 


p 


ft  •  ft  •  ft 
o    •  o    •  o 


p  :p  :p 

o  :'o  :'o  :o 

go  go  go  go 

O+J   CJ-W   O+J    O+i 

t  fit  fit  ct  c    ■ 
S»(i)«;o*4)Ooo 

SSgSgSSp^H 

<^     <d     <J     <}     oo 


<1 

x      os      o      ^      cn  co  •q-LOccr^xoi 


H 

i* 


236 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siaxreq— ^onpoid  repini 


•}89j— indap  I^OJ, 


•;aaj— i^dap  \\o 


£ 

o 

I 

fSg 
09 
3 


f 

o 

I 


ran^p  9Aoqi3  opn^jv 


^98J— \9A9\ 

■B9S   jAO\sq   opn^jv 


199J— 

pg^jpngd  ssau^oiqj, 


•^aaj— do;  o;  q^daa 


&  • 
cs  o 


CO 


c3  c3  c3  C3 

oooo 


cocococo      JO 


ia>      co<n  • 

.      .  JQO         OMt       _ 
i  i-H  CO  CO         COCOCOCO         CO  CO  CO 


CM  <M  CO  CO         CO 


CO  ^H  t-h  CM  CO 


NWN        CO- 


CO CM  00  O        t*        'Ji        CO'OOCM©        t^l 
O  O  O  CT>        ^h        <M        CO  CM  -*i  CT>  lO        co  < 

oo  oo  oo  t-      oo      oo      oo  a>  co  r-  oo      r^t^oooo 


a 
o'd 


(M  CO 

fl  fl    '.Art 

O  O  fc»  o  o 

Hill 


rHCNCO 

fl  rt  a 
o  o  o 

5^3  3  3 

Sill 

coPhPhPh 


o-dTJ 


t-  CO 


(/>   CO 
C3  03 

OO 


IHHHrtOHO 


CO  CO  CO  CO  CO  Tt<  CO  • 


i-HCO<NC0 

d  rt  a  A 
o  o  o  o 

ill'll 


00  00  iO  O  CO  iO  iO  ' 


io  t^  r--  io    »o 


00  CM  rH 


o  o  o  o 
££££ 

c/T  co"  oT  c/T 

aaaa 

c3  c3  c3  c3 


«    oi 


o      o 


p!     tf 


6 

r-l<NCO<N.-H      •      •     ^ 

o  o  o  o  o    .    .    g 

,  a>  <p  a>  cp  ®  co  <2    3 

■  .2.2 .8 .2 .2  Soj   s 

."S  .t*  S  .tS  .t;  t3  t3     o 


•b  :b 


- 

o  . 
a<3 


ooooS^s*     3  <»     ®  c» 

ssssssga  a  a  a  a 

OQOO<!     <i       <J       <d 


o  :b 


SSI 


®  0>  CD  ® 

aaa" 


aa 


a 


CM  CM 


cp  S-rt-r!  °  °  °  °  °   -0  ° 

as©«33333  ►*  3 

<j     pjpJOOOOO  ^  o 

r-     oo  as  o  i-h  cm  co  f    io  co 


it 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


23r 


- 

CC 
X 

I 

© 

as 

fcT 

© 

1 

DQ 

9 

3 
r 

t- 
c 

s 

0 

00 

a 

cn 

s 
r 

t- 

c 

g 

X 

1 

<M 

O 

OS 
(-T 

S 

X 

d 

5 

© 

© 

U3 

00 

8 

- 

t 
'_ 

c 

y 

1 

oc 

s 

02 

•d 

a 

03 
DQ 

'5 

3 
CO 

3 

0 

— 

X 

- 

c 
o 

a 

& 

£ 

K 

i 

BO 
X 

cm  t  -  y_  ~  ~ . 

SNSOO 
X  cc  rr  c;  oc 

0<NO 

N  IQ  i-l 

bo  oo  a 

CM 

Hiom 

tONO 

oc  ooo 

CMN- 

ocoo 

S    ?5 

oo      oo 

5 

io 

So 

— 

Cft 

I- 

OONO^TtiaiK- <Cl'^CON-N."?>CO-«Tr'COTt<Ci''I'aCNCC-<rGCSN-cON 

c  t^  n  l~  i-  s  c  -^  m  ?:  n  n  u-  c  l-:  n  n  c>  >■-  n  u:  or  c  c;  c  c  c  l-  c  rn  it 
o»-H»-*>-ii-iooc^HOi-ii-(Oi-HOi-(-HO«ni-<t-iOi-iOi-<«^-.>-ii-ii-i^ 

cm  cm  Tti  n-  n  co  Tf 
■"*•  tt  i-H  co  io  ia  co 

cd  t>  re  cm  cm      «      us      "5  co 
n  io  n  co  co      to      co      cm 

^•oeoi-ico*&'-*^~aai-i9SBCococD^a>cD(OcDi-icDCScoc9^iioooco^<eoac>aocDeQeot-«o 

~~:c:erovvvcovcocovcOTrcocov^coco^covco^cocococococococococococo 

T  CC  N-  CC  CC         CC         lO         ION 

cm^j-cmccco      co       co      -<rco 
co  co  co  co  v       CO      CO       COrf 

3 

i-HCO<-l 

SSS^^^^gs^^^Si^SSS^^SSS^S^SSS^^S 

(N  C  N  C  L-        O        t-        oc 
CM  CM  CM        CM        CO        CO        CM  CM 

cc-iaxxN^cw^^-L-'/c^c^^NNincNofficoiioc'flTjr-OTt^c: 
ocOffiOxcccrc-t^t^c;i>XNNL';occxL':Nr-~~j:--.L-cMC'U':fqOH» 

0CXN*t-0CX©XO)^M»N00NN««NNXNXN«NXM0C««««««XN 

IN  l:  f)  C  C         CC         N-         ION 
t-CN^O         OC         00         OS  *ri 
N  CC  t>  t-  OC        N        n        N  Ci 

- 

P 

c 
5 
IE 

0 

z 
— 

> 
B 

c 

a 
P 

z 

M 

B 

5 

e 

P 

C 

r 

C 

« 

2 

a 

C 
-- 

s 

X 

0 

re 

i 

a 

= 

a 
- 

p 

c 

J: 

a 

2 

z 
— 

P 

C 
a 

C 

i 

p 

C 
- 

c 
— 

B 

5 

9. 

A 

a 
- 

1 

3 

X 

p 

c 

o 

— 

C 

C 
a 

-~ 

B< 

p 

5 

— 

C 

X 

P 
a 

l 

o 
— 

cm 

= 
c 

I 

— 

z 
P3 

= 

c 
a 
P 

1 

: 

c 

— 

cm 
§ 

p. 
P 

l-H 

c 

- 

c 

c 

c 

p 
c 

a 

= 

c 

--> 

z 

c 

z 

X 

CO 

= 
c 

p 

1 

- 

p 

c 
p 

- 

c 

c 

X 

I 

a 
1 

NOV 


co   ovisN   n   ia 

TK     OClOCO      CD      CD 


CD     iO     MwOMOMNiS 
CD     CD     CCCDN-iOiO-fCO-* 


©   C  C 

pTs  pT 

©  ©  © 

££  S 

EE  E 

o  q  a 


IXOL'H 


Z      Z  W.      "•  « 

•m,        m,  6        6  6 

"©  ■©  z  z  z 

»>    •>  cT   ciT  gT     gT 

*     ><  fi    fi  ft       Pi 
OOO        o 

§  S  ^  Ch  Ph    e- 


o      o 

z   z 


°    dodo  d    do    d  ooodocoZ  Z 

d  ZZZZ  Z  ZZ  Z  ZZZZZZZ---  j> 

"^     ot"  oT  c/f  w"  oT    cc"  0?    of  co  to"  bo  «T  wT  kTib  O  © 

•■"■B-B-B-JJ  t!  -a-B  -B  -Siif'S'if'if'Sg  § 

ftc3e3c3c3  C3     C3c3      c3  c3c2c3c3cSc5c3G  5 

O      ftp.^C,  Q,     ftp,     P,  p,piplPlPip,Pi*  « 

P->    C/2XXX  X    XX    x  xxxxxxxS  S 


z   z 


£   £ 


o    •  o 
*©    !"© 
>    •  > 
©    •  © 

©  ! 
>  • 
©    • 

a  : 

=3  :«8 

•8  : 

2 

a 

!     J* 

i    E 

•      PC 

— 
c 
c 

- 
& 

— 
E 

i 

- 

c 
c 

X 

z 
c 
is 

E 
C 
| 

PC 

EC 
k 
d 

i 

3£ 

IX 

- 

a 

c 
(- 

PC 

K 

c 

PC 

(- 
- 

c 

i- 

- 

Z 

a 

a 

c 

- 

- 

a 

B 

c 
Z 

z 

■- 

- 

a 

a 
- 

- 

■       V 

o  :o 

c<  °  e  c 
©*»©*= 

o  : 
■8'S 

s    o 


N     ftp,p,ft    ft    ftft    ft    ftftftftftftfto     -     e'eo     ©© 

3    |  §£c£   8  S8  8  S  §  8  S  8  8  §£   «  S^gS   £S 


io    con-    oc    eoHN««me    n-    oc 


238 


OIL  FIELDS  OF  CKAYVFOKD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


spjJBq — pnpojd  i^iui 


•%99l— t^dgp  i^o J, 


189J— itfdep  HO 


a. 

O 


58 

© 

o 


uin^p  QAoqB  8pn^i^y 


•^aj— \d\Q\ 
B9S   Avojaq   epn^pxv 


-;99j— 

p9^J^9U9d  SS9Ul[0mX 


"J99.f— do^  0^  md9d 


g  o  a>  o3  ac, 

cc<2  «■>  ^.2.2 


S* 


53  © 


^5 


OOtO'OH 

«hhO 

OS  00  OS  00 


1^  N  ■*  1^  1^  iO  "O  -f  iO  rt  CO  CO  lO  [^  K5  O)  M 

coNHTtuNiocofwmtmiO'OM'*'* 

i-Hi-HOt-H©i-Ii-I©i-I©i-I©.-I©i-I©© 


COCO<»fOCO'0'*ffliOO>WI-i 


co  io     ■  os  co  m  t-H  i 

NH       -r-KNCOTfl 


0000-HC0CO©O5^'O©CNCN>rjcoia^H00 
000COS00OS0000O5  00  OS  00  OS  I-  00  00  OS  OS 


iHNM-HCOH 


rt  CO  pH  CO  iH  CO  M 


333333  13333333333 


pSp^pspspsps 

:p2p2tftfpitf  pspspsps 

§  5§ 

>o 

S 

1 

TJ1 

1 

s 

«3 

6 

6    d 

6 

oo 
6 

6 

CO 

6 

d 

d 

£  £  fc   fc 


£  £ 


SSSSSSSIS 


«     a     o 
t3    t3    t3 


<i 

ti 

M 

ti 

PS 

X 

PS 

PS 

PS 

■- 

r~ 

oo 

OS 

CN  CN 

<M 

CI 

Id 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


239 


spxieq— ;onpojd  vepiui 


•jaa;— qidap  p^oj, 


■}3aj— q^dep  no 


•498j— auBjd 
uinpsp  9AoqB  apn^T^y 


J98J— I9A8I 

Avopq    opn^T^iv 


laaj— do j  o;  iwdad 


°  ij 

<d    .  c 
a>    ;  o 

Ssl| 

JO  <s 

+j    TO   »" 

■as! 

pebbles 

Coal  226  feet 

Gas,  924  feet 

Quit  in  sand 



1 

A 

■# 

(- 

5. 

c 

Ss 

r 
CO 

OS 

CO 

0) 
<a 

X 

OS 

»-~ 

"Is 
"3 

C3 
en 

#g 

±3  C 
53  "C 

0? 

•  ©  • 

!o    ! 

:8  : 

Ml 

Ss^'S     ' 
US*- 

coO 

o    •  >© 
•XI 

= 

o 

■p-POiooioio 
be  be- ' 

33 

S 

3 

CO         ©       •(- 

3J 

OS 

1  - 

OS 

X 

OS 

- 

OS 

CO 
OS 

r 

-r  t 
OS  3- 

O 

OS  t~-  OS  »-H  o~ 

-H  CO  T  UO  IC 

KSiOiONMi 


)MOOMN«CrtM«NHt^W 


HOOM         OOC)6cOI^CO^^CC(r^OSOI:^-iticOOiCCOCD>0'^l6Ci.'Or--^t,lO         t— 
-h©©        OOOOOt-h  ^h  C-h  ONOh  OOOOOOOOO  ©  ©  i-h        O 


iCOCO-fCO'^IMTrcO'ti''*1, 


ioti<0'*io»'VHOi.o(oiCNa 

N  N  t^  K  -^  X  re  re  —  X    -C  -CMC-. 

asascscsosoooooscGaot-ooooosososcsoscscsoscscsosa': 


-  t  -  O  T  CO  i^  to  CC        OS 
•  UO  SO  O}  IC  CO  !C  -f         ■— 


i-H  CO         1-H       !  CO  <N  CO 


5>-H.a 

03,0,0 

£  o  o 

COPnPi 


°5 

:  g  g 

i  o  o 


<m    '.cn 

«  :  c 


.5  >>5 


II  :| 

'  •  B  5  :  5  5>,  .' 

2  <? O  2  §0  (SO  C?3  OOOOO  03  3  O'^g  v 

■    'pipi    \<£w  & 


;  hn 


M 


T-l 


,£_;    w     w    w     w     ■—-    w  ^  ^     v^     cv 

or^'w  o  _£  °  .2  °-2  o  r0  'O  'd  'O  'd  tj  o  cO  o  is 

Pico  :  pi  co  tf  co  Pi  co  Pi  '.  ' 


r-l  O       OS 


t—      OtONHOON      t>-         OS 
OS     I^I^O^hOO     o       o 


^  ^   ^  2  fc   ^   ^ 


a>    <o    <a 


0)0)0) 


•.OOOOO      ^       - 


0)  O  0)  o  o 


a?    ^3  ^3  s  Z 


co   co   co     co     co     co   SSSSSco 


■2-2       © 


C^O 

sz 


o     . 
■rt  o 


o    o 


^H  d       CO 


c3     >»      >» 


c_ 

o    o 

OO    P3 


05  0) 


pq       CQ     ^(ntLntsnfcQ     O       O 


240 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sjaxiBq— ^otipcud  teprai 


}99j— q^dgp  p3;o  j. 


•}88j— q;dgp  no 


•198J— OU'Bld 

unn'Bp  OAoqB  apnmjy 


aaej— I8A9I 
■B8S    .Auqaq    opi^i^y 


199J— 

p9^a^9U9d  ssgu^ojqjj 


•}99j— doi  o;  q;d9Q; 


^  S &  «  g© 


S55 


■rt  o 


s> 


>  Ol  Oi  C5  00 


0? 


ftp 


CA  C<i  <3>  00 -&        OOOiOfO'OO^Ht^O'VQOiOM'iOO!        CN  Oi  >0  i— I  CO  CO  cn 

,-l,-IO.-H©  f-H  Oi-lOO©r-l  000.-l,-H  00.-IOO  ©  CO  lO  »-H  O  1-1  O 


00  00  i-t  <N  CO  ONiOTI<iOO!DOiMOcOOOW<OU5H  00iHU5O)NN00 
CN  -fi  CO  OS  CO  NCOai«3'<(,t^CDCONNOOOONdlO'OCO  lOi-lNN-*  »ffl 
CO  CO  Ttl  CO  Tt<         CO  Tfi  CO  ^f1  -en  -3<  CO  Tp  t}<  ■»*  CO  CO  •«*<  ^  CO  Tfi  Tf         -^i  00  O  CO  ■*  CO  ■"*< 


ONOOO        CO  CM  CO  -H  < 
0000O500C5         OO  C3  00  OS  < 


iNOlOMOOOOOOMNO         MtOOWNNI 
i  tJ<  CO  CO  CD  CO  CO  f~  CO  -<J<  CN  <N  O         K5ONNC3  00I 

i  o>  03  OS  as  as  oo  oooi  o>  oooj  ct>  ©  co  •>»<  oo  ©  oo < 


o  o  ,  o 


a>  a>  co  .  co  91  to  oi  in        cc 

.s.a.s   >,s.a.s.9.s^..s 


>  O  O 


cgPh 


O  O 


■oo^o'd'tio'Oo'tf^'o     "o 


j3  o  o  o 

CoPhPhPh 


O      *     N     ffl 

O)    o>    to    to 


~H  CN 


O 

o       r_r 

o       3 

P£        P-, 


O      O  ■*  "5  "-1  ®  N  M 


o      o    o  t3  ^3  d  "c!  d  t3 

S-|  H       I-.   0)   ©   O   ©    <P   CD 

Ph     04   PU  Ph  Ph  P5  Ph  P5  Ph 


iH      ©      i-H      .-H 


55  55  fc  55 


^2gS 


6  o  £ 


<g  o  o  o  o  o  o 


,3  A  A  A 


1* 


'3 

pq 

'3 

pq 

'o3 

C3 

PO 

•eS   •c3'rO>l!3ia'^lld   .23   .2   .2   .23 
PQ    PQOOOOOO    Ph    PR    Pm    Pt, 

c3 

83  £ 

CM 

CO 

iC 

co    t>-  oo  ©  o  i-i  cn  co    •*    io    co    !>• 

CN  CO      ^f 

BLATCHLEY] 


TABLES    OF    WELL   DATA. 


241 


IS? 

100  ^ 


.O  03 

«3fe 


o«£v 


"So     J22S 
£  g     <o  oo  t» 

■Jg  O         03  03  03 


2b2 

3       3 


^       -  ft 


o  o 

COCQ 


01050 


NOMNN 


£gg 

i— i  O  .— < 


CO  CN  iO  O  CO  O  MNNNNNNrHrtOlOOHNMOCO 

i-H  »-l  ©  ^H  ©  .-H  OOOHOHHHHHOOHfflffiHH 


COO 
CO  TJ< 


as 


•  OKNTfWr-OiH 


CO  CO  -"t1  CO  ^  CO 


00  -^O  C-  CT>  iO 


NNHOU5 


dNO^OUJiON      •  © 


cn  cn  oo  io  io  oo  co 


MOOKO 
t^  CN  iO  CO 
i-H  CO  CO  CO 


00  «  00  CO  «0  »Q 

00  00  Ci  ©  ©  © 


•  cocn-^ooio^cniio' 


OOO) 
iKOH 

lOiocoo 


oo  o  oo  oo  oo  oo  oo  c 


KC  CO  t^  M< 

ooo  oo  oo 


o  o 


o  o 


.0,0.0 

ooo 


sas 


,0  03,0,0,0,0 

o_j-  o  o  o  o 


!  a  a 

>  o  o 

)  co  co 

i  9  S 

>  o  o 


in  o'D'd 


£  '• 

ot3  ox? £  o 


tftftf  : 


=3  >>«-  ■ 

CQCO     .W 


oo    ©r-i 


io  ©  t^ 

O  -HO 


iftCNCN  ( 

COO)d( 

TP   •<»<    TfC   ■ 


CO     CO     00 
US     US     iO 


iiOt^i 


HN    H-*MO      O 
O  o      O  O  O^     ^     ±!     .±3 

fcjz;  !?Wfl   pfWoK 
fe'JS  ,2>.2.2  2    2    <^    -« 

3  9  SSS^rt  sss 

o3  »    «  cd  co  o     o     3^3  3 


i  i-i  ©  oo    us 

°  °.KK   r.    -  fc  fc  fc  » rfrf  j  fc 
9    -    -    -9  999 

o 


<  lOCN 


'  CO 


CO       CO 


g  £2,2,22  2  2  2  2223  2  Js 

3  g  5  co  co  o3     o3     as     co     coc3o3e3     cS     & 

oooSjgw  w  s  s  awww  a  ^ 


.000. 

£  SSS&Sii'g 

•8  Jhw  «■§■§«§ 

03    ^^^        ^^>2 


;      ...;.••   S   :g 

03  03C3      03   03   03   «       CO^    CO  £j 


w  w 

•8  «<3 


00000^    £    6 

22222  ° 


s 

c 
o 

a    co 
&  55 


CO  CO  CO   CO 

S  SSE 

o  000 

o  000 

£  £££ 

CD  CO    CO   CO 


OOO      w 

KfflM  M  =8      "3  =8=<J=8 

CO       CD    CD   CO 
bti    tuptctsc 


aflflS 


3<3<3  «3    Si 

s  c  a   a  3 

O  o  o     o     «- 


ooooocQ  a  o  o  owwrn  w  p^ 


c^     o3  03  o3  r^H 
Ph    ^PhP-iQ 

(N     COrr  lOCO 


WW 

^^ 
fl'rt 

2  22 

WCQO 


(OI>     00  OS  o  ■ 


rH  CN  COrr  iO  ^h 


<M     CO     •ViOCON     00 


N»0) 


#5    DQ 


—16  G 


242 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


■spxreq— ^onpoad  p3ijnii 


•;98j— qidsppnoj. 


•^af— q^dap  no 


S 
o 
Eh 

Go 

o 


T 


mn^p  8A.oqi3  apti^y 


188J— \Q\Q\ 

bos    Avojeq    epiui^y 


•138;— 
pg^j^Qued  sseuipiqj, 


•}98j— do%  o^  qidacE 


StOOLO 
CO  t-  00  00 

saaa 

oooo 


£23 

00  00  00 


coo 

O5  00' 


~    co 

ICi    C3 


£ooi 


§S2 

X   /.    At 


:88 


oOOO-f 


C3   Jh 

,q  o 


£55 


HHHTfNONXN        C»  00  CO  CO  CO  i-H  CO 
(NNM^t-MOcOO 


I  CO  CO  CO  CO  CO  t1  CO         CO  CO  CO^COCOCOCOCOCOCO  CO  CO  CO  ^3*  CO  CO  " 


lOOOMNt  N  ■-    - 

cocoo  irt 

SO  t- 00  00 


O>-0  0000C)i-~~   /^rcCCt^OOHi 
•O  NOS>r  si  i-  c  ■-  si  t~  -h  [—  r- 

000000O300t^0000r'" 


00  00  00  05  00        00  00  00  03  00  t- 


"d  O  c3.c  siS: 

2*}**  c  -<  o 

03     '.  03  Ph  72  Ph 


g 
3  08" 

P3dq 


CO^H 


o  o 

X2   O  03^2X3   C3.0   03.Q  c3  ,Q  C3  .Q  C  ,Q  c3 

«  :  m  £  PhVx  £2  «  £  ps  <£  Ph  :pho3 


CN 


c  o 

CO    CO 

a  g 
S3 

o  o 

phph 


to  o 

-r  r 

oooo 


CM  CO 


<MCO 
i— l  t~- 

00  00 


-t  ° 
03Ph 

If 


j  2®  ^S 
^"S  >  o  © 


oo 

CO 

lO 

CO 

es 

^ 

t^Ol 

£6 

o 

55 

O 

55 

o 

5? 

o 
55 

o 

5? 

o 

53 

o  o 

5555 

IS    CO 

>    CJO 

5.SP 

05 

si 
ttfl 

en 
So 

5fl 
60 

co  co 
be  be 

M)b£ 

z 

d 

I 

£     ZPQ   pq  CQ   PQ     PQ     CQ     pa  PQPQ 


fc  55 


3     3 

PQ  PQ 


SZ 


S^55 


o    o    o    o 
o  o  a  a 

SEES 


S     £ 


s  ss 


Ph  Ph  Ph  Ph 

^i  <%  <%  *% 

O  O  O  O 

'  ^  5^  Jh' 


.2     .2>h 
o    oz  z 


Ph  Ph 
O  O 
55     55 


=3   <3^ 
O   OO 

55  2Z 


II 


°3    «e  «3 


iO  CO     t>     00     O)        O        ^H        CM     CO 'cm        H        (N     CO 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


243 


" 

i*  — 

X  X 
DO   0 

~  r 
C5C 

| 

'- 

X 

- 
- 

r 

at 

i 

- 

OD 

s 

o 

73 

i 

e3 

s 

09 

OS"'- 

00 

J- 

03 
* 

- 

DQ 

£°°c3 

> 

En 

P 

03 

CO 

0Q 
05 

- 
— - 

0! 

00 

c 

1     : 

X 

g 

X 

X 

- 

X 

5 

X 

s 

7 

c  a 

X   X 

N  MO  rt  -  '.-  -    -  r.  :c  i"  /  ONOOnNUJNi-COO«BOO        NTL»,x-r«otZHMiflO 


00W»O(NHgX?:Zr,Z^5MMTrNHHNrtrtOMH0!N»CO         OHHONWNN. 


H»HV»»OH!SHeHNOt»MOt» 

«M^coooc<5''3<-'tf'co-')<eo-'3,c'OTt<cccoeceo 


coco»oooooeocoioiocoi 

1— I  1— I   CN  T-l  T-H  I— I   T-l   F-l  I-H  ( 


8 


SO^NMOiOOOOiOOOOOcOOOMMVHMOlMiOOCtOOlVOO  30  IH-I  N  O  «  N  N  31  B  (>5  »  00 
O  f  3)  n  3  l-  X  3l  T  O  t  O  i."  X  rc  O  K  O  C  C  3  C  C  'i  C  -  C  '"  30  B  «5  t-iOTfiiOSOMMMWOO^"^* 
000O0O00  00  00000000C7J00O5000000O00000O00000000000000000O000O000         00000O00000O000000O50000OJ 


tftfgtf  : 


^q)qOOOOOOO)q' 
O  C  73  73  73  73  73  73  73  O 


:  a 

d 

3 

o 

c 

0 

en 

:  a 

% 

i 

O'o 

■g 

o 

00  00  00 


"»<  r*      C5      00*H  -f  00 
1O00     t^-     I-  00  00  t— 


OOOOOONNB    r~ 


£    £    £  w 


CO  WH  r-H  CONt 

»  M  HU) 

o  o  o  o  o  o  o    . 

fc  fcfc  5?  £££©  ©  oo 

M  ^.i*  44  o3  o3  03     „  „  _   . 

O  ©   ©  O  X2£X1^  4«J  ^j   w 

3  S3  3  33  03  03  o  ©  ©  © 

CQ  CQCQ  CQ  ^^^  3  3  3  3 

.  .    .  .  §§§CQ  CQ  CQcq 


6  6 


'ion  d  d  d  6  6    6    w 
2d6Z.;z;£;z;£  53  sz;  fc 


^  £  £  6  £  £  £  g  fi'  s  fl  pf  fl"  fl- 

vT  -  -  Z    ~  ~o  o  o  o  o  o  o  o 

•S  03©  ^CCjCOCOCOCOCO  130  CO  CO 

3  °  ®  ^5'3'3'C'3rO  -3  73  -d 

W  •     •  .2?©  CD  03  03  03  03  03  03  03  03 

_•  WW  CC2ZOOOPQ  Q  O  O 


£    £ 


o  o  o 
ooo 

CO    CO    CO 


03  03  03  03  rrt  73  73 

■S  £  pr.  £  3  3  3 

13  T3  T3  T3  w  w  n 

W  WW  W  ^H3^ 

^  <#»>}  og  ooo 

CO    CO    CO  rM 
©    ©    ©    CO 


_      ©  ©      ©     ^JS-S  3      03      03  03 
03     03  o3     3     §§8^     *    ££ 


73  73 


bO 


33333  3     3     3 

£££££  6  €  € 

ocooo  o  o  o 
OOOOO OOO 


CO        CO        CO 


t»        00        Oi     hN     M     HNW*     io     ON 


rir.     .     '     .     .©C'©©©  <u     <d     ai 

"i    ^^>Hr^3-§'§^^^^  "S   "S   "S 

i>  Bw!z    OQooooo  ooo 

00     3)Oh        NWTfL'jBNM  Cft     O     T-i 

rHr-l          »-l  T— I  t— I  rH  rH  rH  H  rH       CN       M 


©        .    © 

ft  :Q 
73  :t3 


G-3  3-^ 
o3  3  o3  3 
o  ©  «  ® 
'C  3  "C  a 

i-H        CN 


244 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


IS 

;► 

■  -i-s 

'.  \j, 

-J    5 

CO 

1 

:| 

.      .   CD 

1  : 

03 

a 

• 

00  : 
00   ; 

CD 

.  co  o    . 

ill; 

:  :* 

.        ■  4J 

:  :l 

5    5«n 

•    •oo 

fe  : 

"«8  : 
^  : 

"5 

: 

i-S05  : 

:  :"cs 

"os  : 

rx 

.CQ 

•     .CQ 

:  :o 

CQ     . 

•spxreq— ^onpojd  im^ni 

>> 

ft 

o 

IS  : 

S 

o  ■  • 

/  's 

•  ©    • 

CO 

•%&}— q^dap  ib^oj, 

© 

oi    !    ! 

S    S 

•  C3S      . 

9) 

•CN      'OOCN      • 

•  •  lO  CO  C35 

•  •  CO©  CN 

•  joooooo 

t^ 

;99j— mdepiio 

•  CO      'CO  lO       • 

•  oo     ;  oo  oo     ; 

•^98  j— enBid 

TP  CO  CO  CO  i-l  ©         00  CO  I> 
lOtOiOCOOO)        CO  lO  CO 
i-<©r-I^H^< 

iohooomioc 

O  i- 1  O  1-4  T-H  .-1  I- 

CO  CN  CN  ■*  rti  t^  00 

1— 1  ©  1-4  O  1-1  1-4  © 

ranjep  aAoqe  apn^pnv 

THCN©eN 

CO  t^  •*  t- 

©  ©       CN  t^.  CO 

©  i-H          CO  Tf  CC 

i00)ONN«5ON000CH0(CCCN 

•^88; — jaAaj 

-s<co©oc 

rf  CO  Tf  CC 

Ni>Tticomt-^ 

t^  CO  CO  i-i  IM  00  CN 

rocococ 

M^MMM' 

^co-^cococococo' 

■eas    Avojaq   apn^iv 

S£2£ 

OliONOO'* 

: ,r 

l0  00i-IX01NOiC'W'>J'rHir5NT}l 

•;aaj— 

rj<        1-4  r- 

1-HCN 

CN  IM  H  CO  TJ<  CN  <M 

CN  i-t  lO  CN  lO  CN  i-l 

"d 

pa^j^aned  ssau^orqj, 

HOOOC 

i-h©CNu- 
oo  oo  oooc 

tONNON'*        CO  00  C- 
O  ©  CN  lO  00  r-        ©OCN 

oooooooooooo      oo©oc 

lONMOOOCOlOlOtDlOmi-IOON 

CQ 

•^aaj— do^  o%  q^dea; 

ooioHONiofioHHaoifla 
ooooojooooooooooooooooooooo 

: 

*• 

■      .c— 

,ff- 

6 

a 

i-t     IhC 

rt«      |l- 

N 

COTfi^ 

CprHCOrH 

!  CO  i-4  CO  i-l  Ol  CO 

d   !  d  p 

p)  a  :  p 

h 

a  pi  i 

g  g  d.  fl 

;  d.  ^  0  pi  a  pj 
.  0  g  0  0  0  0 

03 

o    .  o  c 

o  o    .  c 

o 

o  o  c 

o  o  o  o 

55 

CO        .    CO    (/ 

.3  >J.E 

.11  k£ 

1 

S^P 

sill 

'*%%**% 

£3  03£!,C 

,Q£3  03  x: 

S°    '.S'S'S-q, 

©3  3  SS  2)3 

o  «s  o  c 

o  oh  c 

c,i3      o  o  c 

o  o  o  cccc 

'd  0  0  0  0  0  0 

PSCQPtftf 

tftfcotftf  :    tftftftftftftf  :  : 

:  P5  p3  rt  p5 «  tf 

cq  «S  ©  >•  .S  «£ 

«> 

, 

,     ^_^_ 

^^_^^ , 

rHlOlC 

, 

oo 

to        at 

■*r 

i-H           < 

D        00     CC 

00      t-        *o 

co        CO 

CO           CO        CO        t—     r~  r-  t-» 1-- 

r-      t^-        t^ 

•qi        rt< 

Tf>                "* 

Tf<          ^1               ■«< 

I? 

CD    CP 

CO 

03 
CD 

H     lONNK 

1-1        <M           CO 

J      3    J 

2      6    6  6  6c 

6     6       6 

o 

H.    fc  ^^;^!z 

55     55       55 

o 

lO        ■«*< 

CO           c 

6        6 

o                 ~    -    » 

a 

03 

55      55     5 

Z     -d  -d-d-d-d 

*d     *d       *d 

6      6 
55     55 

6         c 
J3       5? 

o        o 

-   pi  a  a  a  a 

^j          03       CO    03   CO    c 

a      ^3   ^3+3^3+j 

d      d       d 

Co        c3           Co 

o      o 

Is     1 

■.      d         3 
A       A     f 

3               «M          «-l     Jj     »-     SH 

www 

.d     ,d 

CQ       CO 

.d         ,3 
CQ          CQ 

*       £     f 

S      Q    fi'fiPP 

odd 

"S    •« 

© 

<o 

:    -d     2 

t>> 

>      > 

> 

> 

:    *o3     "ol 

ps 

0)      ,  CD 

CO 

CO 

•     d       d 

03 

A  :P 

A 

A 

•     0      0 
:    a     A 

0        0 

Pi 

a 

o 
o 

'o 

o 

CD 

a 

03 

-d    I'd 

d    •  d 
o3    ;  o3 

TJ 

§ 

•d 

CO             CO 

V,     V, 

03          03 

0^0° 

03  d  3d 
o  ©  o  2 

1  ii  i 

SoHo 

§5  o£ 

C3+3     d+= 
03  (=1     03  C 
O  03      O  CD 

■c  a  ts 
a&a§ 

*          *       - 

-d       *d     ; 

a     w    f 
•a     «a    - 

CD             CD 

1       £            *        ^ 

03            03 

3     : 
3     : 

3 

**      o    o 

=3       2     2 

c 

i 

-d 

CD 

pq 

-d 

:   «3     ^ 

!     d       d 

M          03             03 

1  i '  § 

Add 

~          CD             CD 

OSS 

<1      <! 

<J        «*! 

Ph        Ph     p 

in    o  ootftf 

PS     A       PQ 

CO 

iC          CO 

Ir^          00       C 

»         ©      ^H  CN  CO  Tti 

lO         ©            t»- 

p<  * 

03  O 

%X 

a 

o    . 
•j3  o 

H 

8* 

I*5 

02 

id 

BLATCHLEY] 


TABLES    OF    WELL   DATA. 


245 


3co3^oo 
£00  ^oo  S3 


cud 
08  O 


n 

^  co 
02  Z 


££ 


"3*3 

cocc 


"3  "3 
coco 


§1 


b£8 
p. ST" 

Hi 


t^  CO 
CiOi 


00  CO  00  00 


5  :S  :§3 


cn  oo      ^     •  m 
oooo      oo 


.-<  ©  .-I  ©  i-H  ©  .1 


0)HrtCllNinO<00'*OK5040®N'*C0^050>OOCOOOCO'*N 

L0Ht^WN(N(»mH(£l(N'»INVXO'rHTl>W10NlOH00'<fO 


■WOOCOONl 


coco-tf'co-^ncococo'*' 


H  lO  H  W  W  rt  lO 

lO  ^  lO  t+  CO  ^-t  oo 
oo  -^  CO  -w  CO  ^i  CO 


COCOCOCOCOCO'^COCO-Va'COCOCO-^COCOCOCOCOCO-WOOCO' 


iOiH<DOJN( 
CO  "W  CO  CO  'V  ( 


lOOrtiOO) 


S22 


$  :32cS8c3 


NN«0( 


lO  OS  CD  00  lO 


iOjflHHHL'S© 

i  00  00  C3  00  00  00  00 


'COOOHOIO 


CO  tp  CO  LO  00  iO  c 


oo  •w  o  ■*  t^  o  < 


>©eO©©©iOCO't,CO00COCN»' 


HNWHMH      ,h« 

a  a  h  c  h  a   \hh 
oooooo      oo 

Jen  en  cn  en  co        en  en 
.9.9.9.9.9  >>9.9 
42  33 S3 3  c3  33 
o  o  o  o  o  o  >-  o  o 


1-H  COl 

o  o 

en  en 

1=1  g 

33' 
o  o 

P5tf 


ICOrHCOtN 


q  B 

C    0 
k  en 

s  s 

,0,0 

o  c 

pips 


as 
if' 

C3C3I 


rH  CN   ,CN   ;  i-i  CO  <-H  CN  CO  "c»  tH  CN  ,-h  CO  CM  r-,  CN  i-i  CN  -h  CO  «-H  CN  CO 

art  ;  a  :aaaflaflrtartrtacfl«flrtGccs 
oo   o   oooooooooooooooocooo 

en     .coeococrcocnencntneneocncocococoencntoco 

^d  ^g  99999G99P|S939999999 
^2  o  c3  3  c3  3  3  3  3  3  3  3  3  3  3  3  3  3333  3  3  3  3 1 

O  0_£-  O  £  oooooooooooooooooooo 


aa 


flCflflCfl 
oooooo 

en  en  en  co  en  en 

flflflfiCR 


•<f     *— I        lO        00     "O  iO     iO 
CO     t—        r—        t—     OOOO     I~- 


s  s§ 


CO  r-H 


■^  Ol      OO  H 


a  55 


„       "1     CO 

d       o     ° 

3     Z  £ 


i-H  >o 


.fa  .fa    «- 


«  o 


O   O      O     Pi   Ph 


6  6  6  £ 
£!5  5?  - 
gfgf  «f  o 
DQ 


ft  AQ  fi 

Pli    P-iPh'    P-! 


o    o    o 

fc  £  B 


ft    M 


t       1    1    D.       L       O 


0     A 


O     O 


p 

i 

d 

5 

o 

S 

Q 

- 

- 

o 

s 

M 

5 

^ 

^j 

s 

d 

a 

a 

a 

H 

ert 

0 

S 

s 

a 

g 

1 

a 

3 

a 

9> 

S 

pq   pq     pQ     Pl,  pu, 


is1 


Ph    PhPh    Ph<1 


2  £   £ 

=5     3     2 


"3     "3 
o      o 


OJ     o        -* 


S5       c$       8     8  Si     81 


246 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


© 

tQ 

I 

1 

o 

I 

I 


! 

a 

CD 

•    03 

!«£ 
;o 

11 
If 

a 

T 

■1 

•     t£t£ 

OS  i-l 

osoo 

:   aa 

:    oo 

•spiiBq— pnpoad  i^iui 

1 

•  CM 

s 

•;88j— ii^dapp^oj, 

-r 

OS 

•00 

jas 

•  •  r^     •  i-i      io     ■  io 

•  'CM      •  tP        n<      •  o 

•  •  OS      'OS       OS      'OS 

188j— tudsp  no 

OO 

o 

7 

o     ■ 

88  : 

•  O  iC  O  C  C^      ■ 

■  co  cr.  o  oo  ■<*    • 

•  ooooocoooo    • 

■  00 
•00 

•  ■a 

;8 

•  :o 
■  C 

•  r. 

00  CO  CO 

WTtOS 

os  oo  oc 

d 

03 

•^88J— 8UBld 

uin^p  8Aoqi3  apn^i^y 

VOtBtBHOliCOONOlfOOOOi^tSHeOHTfHMfflOH         i-l  CO  i-H 
O  i-l  O  O  <-l  i-H  i-H  O  O  O  i-H  O  i-H  i-H  ^H  l-<  rH  H  O  O  O  H  O  O  O  O  O          O  f-H  O 

•^88J— [8A8I 

■B8S    A\oj8q    opn^i^iv 

«0'T'*ciHinNooHioiOHOH®Ti'0)Tfoo:eoiNrHoai      os-^os 

0!00'*NN01i-IMOTNt£Ne01u;L';c<3HNt»'S'OTrNCO         WOOH 
TP  CO  TP  tj<  CO  CO  CO  ^  -#  TT  CO  ■*  CO  CO  CO  CO  CO  co  •*  -v  •*  CO  TJ<  TP  ■*>  t*i  191        tp  CO  •* 

•^88;— 
pa^j^suad  ssaujpiqj, 

OSOfflOOtDOO^OOOOtCtOiOH      • 

H5MHHWHHH           COOHTfN        • 

'  OS  f  (O  l*  M  H  if!  O  «■  M  >J         O       ' 
•  iC  t»<  CO        CO  iC  <N  CM  <N  CO  i-l        CM      • 

3 

•^88j— do^  o;  q^daa 

NMNNOOOVHNCMNOHeOOMOC'iO^Tl'NlOOlXt"         t-  i-l  CO 
00  tp  00  CM  O  lO  t-  OS  i-l  CC 1  tH  OS  N  Ifl  -p  0C   CN  CO  O  OS  ^H  lO  CM  CC  OS  O  CM         rHVN 

oo  oo  oo  as  oo  oo  oo  oo  as  oo  go  oo  oo  oo  oo  oo  oo  oo  as  oc  os  oo  as  oo  oo  oo  as      as  oo  oo 

1 

P( 

P 

c 

V 

_p 
pc" 

i 

a 

p 

c 
PB 

§ 

- 
c 

PC 

i 
p 

IE 

c 

pc 

:  p 

c 

•  e 

c5„r 
H  C 
MP 

P 

c 

PC 

a 

-  c 
mpc 

i 

■j 

p 

)  c 

PC 

s 

o 

g 

c 

-o  l- 

d  p 

c  i 
P  [ 

§? 

) 
} 

c 

c 
-0 

(N  ^H       1  CO  (N  CO  i-H  CO  CM  CO  CM  CO             ',  »-H  CM 

dd   :ddddddddd       ;dd 
oo    .ooooooooo        .  o  o 

COCO       .COCOC4COCOCOCOCOCO              .COOT 

S  2  '.S  S  S  6.9.S.S.S.S      :.S.9 

O  OT3  ooooooooo      'OOO 

tfcd    : p5 Cc3 P5 Pd P5 P4 P5 P5 P3       :g# 

Sur- 
face 
ele- 
va- 
tion— 
feet. 

oooc 

as    r~    tp  i-H    -v    cc 

t^     CO     CO  00     00    cc 

co              as 

00                     t» 

•^<        lO        00        00        00           00     N 
N         00         N         lO         ifl            «3     «5 

Name  of  well. 

M 

■    C 

a 

P 
C 

c 

p 

c 

■■9 

c 

1 

a 

c 

c 

1 

5 

c 

cc 
c 

| 

C 

C 

C 

C 
| 

P 

c 

c 

t 

p 

p: 
c 
!z 

P 
{ 

1= 

K 

>     C 

;  2 

r  -c 

c 

:     r 
t 

P 

c 
e 

0 

s- 

p 

c 

p 

c 

jj 

C 

c 
p 

c 

u 

C 

c 
p 

c 

c 

1 

s 

c 

*    a 
)  |5 

'a 
S 

) 

Name  of  oil  company. 

Brenneman  &  McDonald. 
Brenneman  &  McDonald. 

Brenneman  &  McDonald. 

Brenneman&  McDonald. 

Brenneman  &  McDonald. 
Brenneman  &  McDonald. 

? 

PC 

•c 
a 
pc 

p 

0 

PC 

p 

! 
-  i 

! 

c 
Z 

c 

c 

Brenneman  &  McDonald. 
Brenneman  &  McDonald. 
Brenneman  &  McDonald. 

Rann 

T 

PC 

03  O 

CO-^iO                      CO                l^OOCSO'-iCNCO'PLOCOt--            i-H      CN 
^^        _                     _               ,_,     ,_,     i-H  CM     CN     CM     CM        CM        CN        CN        CN 

§     . 

p5 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


24:7 


— 

cr 

P 

5 

1 

03 

.9 

'= 

_ 
oc 

0 

0 

0 

5 

v 

a 

C 

•  CD 

;  « 

■5 

els"? 
©  >  > 

£  co  a 

c 

- 

c 

© 
a 

c 
2 

-r 

c 
© 

© 

c 

7 

c 
o 
03 
i- 

c 

7 

-3 

5 
o 

o 

o 

B3 

^2 

IS 

o 

q 

CO 

ro 

§ 

— . 

05  05 

— 

OS 

1 

M  O 

i  - 
CO 

O  co 

•* 

I 

Q0 

co  o  oo  io    ■  o  cm 

TfXrtf-      'IOCS- 
00  OOOi  00      -0000 

o 

t  n  o  s  c  i  -  r.  ^  •:  r.  -  :c  /  c  -  c  r:  -h  -5  -r.  r.  ^  ?:  -  r — -jhoioin 
n  n  n  o  c  c  i  -  c  i  -  : i  -  /  ::  : ■  s  c  t  ■*  ^  r.  c  '/.  r-  ;.  /.  n  i-  o  x  cr  -.s  x 
OOi-iOOOOi-iO.-i.-iOO.-iO^OOi-iOi-iO^OOOO^Oi-'OO 

-o  -o  -o 

HCllO 
OlOO 

ON 

as 

MX   i- 

~ 

o;  « 

-    i 

o  c 

iOh-N      • 
KON       ■ 
i— l  i— l  O       • 

■*-*co-*-*-*'^cO'*coco"*'<rcO'*^,v-<rcO"'J,cO"'3,co''»,'»'"'T-'T'co-'rco-*-'tf' 

lOOCl 

>*  CO 

x  o 

C0-* 

HCtCO  IC  X  <M 

IO  CO  CO      • 

cocr.  (N     • 
coco-*     • 

|Q 

u~  >o;  co  t~  x  ~  —  w  i~  i--  co  x  c~i^:i-  x  t-  ic  >.~  o  >o  o  ro  co  ~.  c  c  c  c  m 

i-l  (M           ^H  CM           i-l           r-l           i-l           COH           iHMrir-IC<5i-l(NN(Ni-lNrHr^rt-l 

CM 

lO  00 

OCftOiOCor^. 

i-i  >-i<N      • 

ino  «  o  c  ' :  z  ;  /  -  oi  c  i  •:  -  i.^  i  -  /.  c  ci  -  -/  / 1<  <o  o  x  o  «o  o  o  o 

oj^-^cncxi-c. -c?.  r:  :■  -^  '-.  /.  —  o  i  -  -  —  - -  —  --  i  -  x  —  i~  a>  >c  c  i  - 

00  »  00  M  CO  C>  «  X  X  X  X  K  C  »  00  X  X  Ci  X  X  X  K  X  «  X  K  O  X  CO  X  00  00 

o  =  = 

TCO 

CO  o 
i  -  x 

00  00 

CX'tOKN 
WNOW  OS  o 

X  X  c:  X  X  © 

ooooc     • 

CO  IO  0C       t 
00  00  00      • 

i 

c 

V 

z 
z 

1 

B 
PC 

P 

E 

0 

C 

P 

C 
| 

c 

- 

c 
■c 

i 

V 

C 

- 

P 

E 
■r 

'~ 
C 

pc 

i 

c 
pc 

> 

o 

a 

c 

E 

C 
- 

P 
| 

c 

p. 

E 

!/ 

'2 
c 
pc 

z 
s 

P 

E 
0 

C 

pc 

— 

F 

c 
V" 
p 
!E 

c 
pc 

p 
c 

P 

c 
c 

PC 

E 

V 

C 
- 

ON 

E 

V 

P 

C 

i- 

E 
g 

- 

p 

c 

V 

c 

1- 
c 

v- 

P 

c 

- 

ON 

z 
z 
a 

C 
PC 

E 

c 

C 

E 
D 

c 
pc 

— 

§ 

V 

P 

C 
- 

ON 

= 
C 
ry 

C 
- 

r- 

p 

c 
i/ 

c 

2C 

P 

P 

E 

V 

C 
- 

c 

c 

E 

z 

1 

2 

ON 

i 

cr 

P 
2 

c 
- 

^  C<1  CO  H  ON  CO 

CCCfiCC 
o  c  c  c  o  o 

k  k  tc.  to  m  in 

2  '2  '2  S  S  3 
c  c  o  o  o  o 

p:£pi£pitf 

i-l  cm"  co  ; 

c  i  c  : 

c  c  c  ; 

tr.  rr.  v.     . 

PC  PC  c    . 

S  2  2  : 

o  o  o    • 

tftfp5  : 

m       «5       O     ON 

t^      ic      cc    r^ 


io      cm      io 
t^      t^      co 


o    o    o 

fc  fc  z 


Z     55 


»     £ 


®    ®    u  'c  a 

(so      to     O    O    U 
S!      S!      S    S    S 


i-l         N      L-COC 

•    666  n. 

55ZZ  c 

.      „    «  .  .  ^ 

tM      —    —  —  — 

'S     '©   '53'o'S   £ 


CO     IO     CM 


o  o  o 

!Z5  ^^ 

X  MM 

o  o  o 


o 

0 

o 

o 

o 

o 

o 

o 

fc 

^ 

55 

55 

55 

55 

55 

7 

u.r 

bo 

bo 

CMC 

bi 

bo 

a 

p; 

fl 

d 

PC 

PI 

£ 

a 

d 

pi 

d 

PI 

CJ 

d 

a 

a 

=: 

| 

i 

| 

| 

s 

* 

% 

K    co  cq  pa    co       co    co 


2  2  2 


ppp         p        p-     pq     pg 
3      5  5         5         O    .O    .O 


5       3 
^       ca 


B     P      W 


Pd 

- 

■~ 

o 

o 

o 

Hi 

CD 

0 

o 

0 

c 

c 

z 

Cm 

Cm 

CmC^ 

- 

a 

a 

s 

§ 

a 

a 

S 

s 

CO 

— 

,- 

-- 

t> 

oo 

CO 

a 

pH 

ri 

~, 

— 

ir 

-- 

i  ^ 

_ 

_ 

r^ 

a 

^h  CM 

01 

0J 

04 

CM 

CM 

CM 

248 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•feiajxeq— jonpoad  reiiui 


•}8aj— H}d8p  i-Biojj 


■199J— TflCfep  HO 


OS  00 
00  00 


si 

g 

cat 

i 

o 

c 


ran^p  eAoqe  apn^t^V 


B9S    MOpq   opn;i^v 


pa^Bj^Quad  ssamppu, 


1 

© 

nhoo 

HHHO 

1 

0  00  05 
t-  *f  CM 

OOl-H 

10HCNOHC0P5rtt>MM 

ONMOOCONrHCNtMCN 

i— lOl— IOt-HOi— 1  i-H  i— IHH 

00  CO  O  O 

82 

r  r 

i 

CO 

o 

1 

N(DO>Of  ONhiO 
t^OOOCOOiCOiOt^O 
COCOCO-cTlCO'^-'tf'COCO 

8£3 

TP  CO-3< 

Olt-NacOONINt^OO 
CT>-*l^0Ct^t^l^C0CNlO00 
CO^COCOCCCOCO^^^CO 

CO  o 
COI- 

o  55 

i 

CN 

CO  iO  •>*<  CO  iO  <N 

<n 

00  (M 

55 

ON  COO 
.-HCOCN 

NNOOOOON 

'J'lOOMCBt-OOOMiO 

•;aaj— do^  o;  mdaa 


aWOONXfONKNtOrtOO^NffiTtirtMt^CNOMOMtONNNiO 
'^OiiOiONO(OOCNl'r^Of»NNTti©M'3iMO)01HTt(©VNC3iNi-( 
0000000000O300O3O50000O5000000O500000000000000O5000000000000O> 


o  o 

CO    CO 

a  g 

•s-s 

o  o 


-2  2,2 


(NiHCNMHCNMHCNhMiH 


lllil'llillii' 


I'd  o' 


,  Tf  i-l  CO  T-l       ,CO  CN  • 

:  §  §  §  §  >SS. 

o  J3  o  - 

#02  Ph 


:k 


O   O 


tftf 


3  S  ^  cS  fltg 

*-'  m  rr^  k^  /-s  ^n 


iO     03  1000-*     o 
t*.      COt^iOCO     CO 


s  s 


odd  6°    o 

6?      W-Bfsfjkf    ri*T 


■B    13T313 

o    o  o  o.-    .  ■ 


55    55 


£    £ 


S.   PI  G-* 


S* 


•43  o 

CO 


Ha 

Hi 

Hi 

Hs 

1-5 

g  £££&  S 

PL| 

Pi 

Hi 

1-5 

<M 

CO 

IO 

CO     t—  00  CT>  O     t-h 

N 

CO 

IO 

I    " 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


249 


+^  o 


o 
o 

£ 
o^ 


ftp 


So 


NH 
05  05 


JiOOOnOtONONNN        O  O  00  C-.  Oi  CO  Oi  if3  00  t^  r*  OO  O)  ■*  CN  CD  1 


I  O -i  ri  ©  rH  r-l  © 


'©©©©rH©©©, 


©©©rHrH 


MN(NNO)N00rHN(Dn<MiHNNNr-c<J<O5 
010  00NO)(ONONOOtOnONe«!D 
»hOOOOOOOt-iOOOOO»-iOOOO 


NOOHiOTDOl 


II--  lOHCSCOHNHlONCOOSC<lT-ltDOO'W( 


©NiCrNMOlCOWOON        dMOOOMO)C06iO(00>!OtDO>N'*00000 
eo  -^  -cp  co  ■'j'  co  co  •**<  co  eo  ■>»<       -f  ->»<  rt<  •*  -a<  co  -^  -^  ■*  CO  CO  CO  "*  CO  ■<»»  ■*  ■*  CO  CO 


TfOU5HO)iOOOCOO«T|i        ■WOt^OM(N'*c»rt(XION'J<NMO!U5      -CO 
rHCN  C-  <Nr-(  CNrHrH  H  CO  CN  rH  00  CN  CN  H  UJ  (N  O)  IN  CO  (N  H  '.-I 


38 


OOtONiO'nOOlNNl'OH 


©t-CN  -"J"©, 
i—i       Nhhi 


■iSNso^aoov 

NhShnOMOO 
©OOOOOOOOOOOOO© 


•  O  CD  CM  ,-H  CN  ■ 


■<»<iOmCN00CNrH-<fCO< 

HHIlHMn-Tr.;    ' 

00O)O3O5O)O5ffiO>OJ( 


nO(OiOiON(NOCON 
-    "ICOSDNOhOOO 
1  CT>  00  © 


)  OS  ©  O0  ©  < 


N  CO  Tf  "-•  CO      .CNCO—ICNCO       rH  CN  CO  _i  CN  rH  CN  , 


aa 
11 

Pi  Pi 


333  :3333s 
ooo  .ooooo 

222  cs23333 
ooo>-ooooo 

Pi  pi  pi  cc  Pi  Pi  «  Pi  tf 


3  3 
S3 

o  o 

Pi  Pi 


flflfl 

OOO 

aaa 

ooo 

Pi  Pi  Pi 


a  5 
3  3 

o  c 
P3Ph 


^.a.s.s 

03,0,0.0 

J-  o  o  o 

m  Pi  Pi  Pi 


IHM 

I  PI  PI 

i  O  o 

aa 

11 

papH 


CN  CO 

a  pi 

o  o 


.3.3  ^3 
,0,0  03,0 

o  o_>2  o 

Pi  Pi  02  Pi 


o  o 

,    CO   CO 


CNCO. 

pi  s  a 
ooo 


.333 
<s"33  o  ©233 

^oo'd'Oooo 

SpiPi  :  :pipipi 


iCNCO  '.  CN  CO  rH  CN  CO  CN 

13  3  ;  pj  el  pi  pj  pi  pi 

>oo  oooooo 

>  co  co  .  to  w  to  m  to  m 

!  pi  pi  333333 


o  o  o*d  o  o 

pipipi  :pipi 


,0,0,0, 
ooo 

PiPiPif 


2    8 


as  o 


s  2  §  §§; 


CD     CN  rH        lO        t>  CO 


r-l  CN         CO 


a    a    a 


£  £  rS  £  £ 


ooo 

fc  ££ 

aT  ttToT 
o    oo 

a  £a 

r3      ,3.3 

ooo 

3     3  3 

a  aa 


do  d  -  ~  ^ 

£2  £    o    o    o  o    . 


CD   CD 

ooo 

aa  a 

,3,3      r3 

ooo 
3  3     3 

aa  a 


■a  S 

<=>  5 

O  to 

I;  a 


°£   £ 


o  o 


CO        "        W    W  u    v  u^ 

O    O    OOWN      n 


§   si    I 


Q     Q     ft 
ooo 

a  a  a 

<g  eg  <g 

3       3       3 

a    a    a 


pq      pq     pq     pq     pq     pq 


<<J     «8 


a    a 


s  pq  pqpq 

2  ooo 

PQ  a   aa 

00  Ol     OH 


pq     pqpq 
o      o  o 

a   aa 


CO  r-l       CN       CO 


3  3 
o  o 

CO    CO 

II  2.2 

,3  3  3,3 
chEHPhQ 

CN  CO  rHCN 


3  3 

03  03 

pqpq 
-co1 

CD  CD 

Pi  Pi 


250 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spuBq— ijnpoad  i^ui 


laaj— i^dap  p3iox 


<D 

•  r-l 

o 
U 

I 

o 
© 

o 

o 

o 

e 
v» 


•;aaj— i^dap  no 


uirnBp  aAoq^  apnmxv 


•}89J— I8A8J 

■B9S    Avopq    epn^piv 


isss 


0<N  CO 
-r  t  iO 
Oi  03  OS 


■5  :« 


20>0  DiO 
^05  05^05 


OOIN   ® 
00  OS  00,05 


CJOlOi       o 


o>o 


O   03 

^    te- 
rn   > 


*2 


ifliCOOfflN        »C  r-H  10  ■*!  10        <N  (N  N  Q  O)  N  rt  ih 

onoccNocw 

OOr-n  OOOOOOOOO       0  0)000       OOOOiOO^HOi 


«iOO«CO        0  0:00c 


00-*^-iiOCOCO>OiOCNti-00        lOOSiOtOiO        WWOOhhOOOOi 


pa^j^etiad  ssetupnix 


•jaa;— do;  o;  i^dea 


,  i 


Oh    • 
C3  O 


"*3  o 

CO 


rtOOMWOWOOOJXiOinM  CO  N  00  X  O  OOOMiONN© 
Nf  lOXO^mf  NNVlO  f-  00  I  ~  00  00  OCcDOOCDOidO) 
Oi  O  00  00  OS  OS  03  OS  03  OS  O  Oi        Oi  03  O  05  OS        03  OS  OS  O  03  OS  OS  OS 


CNCO 

a  a 

o  o 

d  ri 


iwtf 


g  g 

3  3 


O  O  o 

:  :« 


9  9 
S3 

O  O' 

P3tf 


d  d  a 
000 

01  to  m 

d  a  a 


tftftf 


N  CO  ■*  IN  CO  CO  ' 


c  c 


d  d 

o  o 

.-/     T: 

R  R 

33 

O    C 
XC1 


in  in 

r  r 
o  o 


G3  O 


•/■.  co  -/• 

>— I  os  t- 

oo>» 


<N  t-CM 

0000} 

Tt<  10  10 


CO  00  CO 

000 


R  R 
o  o 

C/3    1/3 

9  9 
33 

o  o 


o  o 


0000    o 

>^>%>%>^  >^  o3  03 
»  »  ©  »  ^  >  te 
42  4^  43  jO    42    -5  t3 


o    000 


o    o 


^3  t3  ^  T3 

t_  t_  J-  s_, 

Cj  c3  c3  c3 

£  £   £   £ 

H  WWW 


3  3  a  3  ♦§ 

pq     pq  pq     pa     M 


•d  -d  o3  03  03  03 

S  03  pafQfQfQ 

ft  ft  .j^.^j^j     000          0000       o 

*  ^  03   03   03   03     4=i     rd,d           44     45^43        43 

^  £  PStftfP^  o  00      o  000    o 


000 


i-H         N      CO^lOC     N 


O       rHNCO 


CO       t^.     00 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


251 


o3.o 


05    ^ 


-  •  I 


ffioo^; 


ft 


C3  O  c3 

0  550 

ft 


§M03o3 
CO 


1  03,03    . 

)  r--  r-  .03 

IOC  oo  *— 


00    j^OO 


OCO     C  co  C 


£oO£ 


coCco 


■*(CO  CO 
O  l~  t-»  00 
OC  00  00        00 


00  CO  CO  (M  CO    -'.NHTfNCO^^MHOCtCOi 

00  oo  tji  t^  c~.  ■  -  re  c-  c  x  oi  — .  —  o"  :■:  c.  «  o  h  l 
0>0>0>0l0>01O0)OOO01OaO©O(5O01O0>0)O01O05OO 


CS  CN  <M 


iiO««iC«i 


)NNOOC»cO«OHtO(Nt- 


OfHHH 

--©oo© 


iOTj<io»c^rio-*l»0' 


--C  i~  ~       -i:mi-  i- 


"f   CO  "*! 


I  O  i-l  OS  CO  lO  C5  I 

iOOO)00)010100)0)0:OOn 


§S2 

OV05  0S 


CO  Ol  lO  c  oo  00  o 
t-Nt-ONtDO> 

00  OJ  00  OS  o>  00  00 


—  .3  •.£ 

o'Coo'Co 


<nco<ncoCjJcocnco<nco 

oo    .ooooooooooooooo 
ic  in        moioimiCKimKmmKmoiKm 

5  5  -5  5.5.5.52.52.5  5.52.3.5.5 
!a  3  o  2  3  2  2  2  2  2  2  2  2  2  2  2  2  2 

o  cd OOOOOOOOOOOOOOO 


o  o 


S  8  9 

o  o  o 

m  m  ot 

o  o  o 


;  h  a  a  h  h  h 

,  o  o  c  o  o  o 

tn  t*>  xn  m  v  m 

•B  5  5.5  5.3 
o  2  2  2  2  2  2 

'd  o  o  o  o  o  o 


w    w    o 

00      CT>      00 


6  6  6  6° 

£  £  £  &     55 

1  1  1  1     "& 

CO  CO  CO  CO         ** 


o      o 
55     55 


,-H  <N  rH 

6      6      6 

55     55     55 


iiON'fl'roN 


B     ffl     W     M     (D     fi     fi 


fH  H       LOW 

6  6    o  6hh 

£\       ^^^oo 

..       -...nt^OOOOOO 

.g  .g   ^^^^55  55  55  55  55 

03  C3       C3   <3  J^  ??  ssT  sT  sT  t>T  N~  N 

£  £    ££3-3--^^ 

^  ^  ^  1°  2  2  2  2  2  2  2  "h 

pu  W   WHZ^cocococococo 


o  o  o 
55  55  55 

o 

55 

03   0)  03 

"3  "3  "3 

03   03   03 

WWW 

■8  ,2 

03  PQ 

•2  -d  .2  .2 

£  tf  o  o 

i-l  CM      CO      T 


PQ      PQ      PQ       pQ      pQ  pQ  2       2OOri*ic'02c'o02 

3    3    3    3    3  3  2    2  2222222222 

sa^^S  a  oo  005^0000000 

""cO        -^         >0        Jh         CM  CO  ^         55     tONOdO)OrHNCO'*iO 


ooo  o 

222  2 

ooo  o 

HNCO  -^ 


252 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq— ;onpojd  i^prai 


•199J-  q^dap  \V)0  j, 


•^88j— q^dap  no 


© 

o 


^aaj— euBjd 


•^89J— I8A81 


paiuxjatrad  sseujpiqx 


•^89j— doi  o;  q^dea 


«L  ©  i    ■    I 

co*5  ©  >.2. 


^06^ 


"3  ^ 


J§  00  00  00  00 
O  03  C3   03   03 

550000 


ft  ( 


lOO^HOOOOO 


CO  "O  00  t^  N  00  OS  CO  f 
Oi"*lOOJr^.-l.-ICO(M 


Tf  ic  r>-  <© 


'O5O500O300000000 


i-H  e^  co  r-t  co  cm 


a  :  fl 


o  o 


o  o  o 


.5  >>3 

O  C3.Q 

PhccPh 


OOOOh 
t^  CD  t^  iO 

oooooooo 


f£00 


OOtDiOIOiOOiOOOOOtONNt-iHtOONiJitOCOlSOO 

ooNotDnoo<OHoC'Hioio©ovooiO(OTfNn> 

,-1,-ii-ii-hOOOOOOt-iOOOi-hOOOOi-h©© 


'lOT)>l0Ol0NINTtiMC<5m0K0N00(DTrNHM 
"~       lOO^VCOOHOiHTticOKSNlO 


^NrtifflOOliOOOOO 


Ol  U5  O  00  O  ■*  115 
HHHUJlJlNH 


OlONrfiOOCO 

-    55  »o  >o  eft  cor^ 


0000000000©00O5Oi0000Oi000000O>00CT>000d00O> 


.(NMHNC3H      ,<M 


JJJlgjJ  :J 


J.sJ 


o  o  o ' o  >)  "o  "5  "q  S  o'o  o  oSIqIqS  O  cs3S 
'd'O'doooooo'Oo'C'Oo^oo'd  »-  o  o 

:  :  :tftftfp2E-ipd  :#  :  :p5p3pc5pch  :copsp5 


CO    O    Oi    o  ■ 

11}     N     ^     UJI 


iO    o      t~- 


CO  ,-H 


o  •    ^      •    •  o  o  o 

^  £  £  tt**}^ 

©  ,2  .2  3.2  ©  ©  © 

"3  ft    ft    ftft'S'S'S 

©  ft   ft    ftft©  ©  © 


o    o 


(N^H 


55    55 


o      o 

55     fc 


M       M    M 


o  o 
55  55 
af  aT 
ftft 
ftft 


a   a 


£  £ 


a   a 

©      a> 


ft  • 

C3  O 

S55 


5° 
©^ 

CO 


a    a    «  a 

C3     C3     03  03 
Wi      M fc£  SI 


Q       Q    fa    fa    fefaOOQ 
t—        oo    05    o    hntohn 


O      O    O    fafa    £ 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


253 


a 

0 

& 

'X. 

il 
:•§ 

"© 
© 

"3° 

CO 

Gas,  846  feet 

Gas,  848  feet 

Gas,  851  feet 

Gas,  848  feet 

Gas,  861  feet 

Gas,  847  feet 

Gas.  844  feet 

1 

c/T 

C3 

0 

II 

<N  -^ 

io  m 

oooo 

a  a 

S 

o 

o 

lO 

>>      OOOOOiOOO»« 

ooo 

o  o  io 

oo 
35  o 

3 

35 

OO  CO 
iO  00 
05  05 

1 

o 

ooooo 

-H  05  CO  CM  00  i-H 
05  00  05  05  00  01 

1 

3 

OOONOCIMOON 
■>*<  iC  iO  -<J<  CO  "f  •«*' 
00  00  00  00  00  00  00 

no 

p 

00 

iflNO 
tr  lO  "^ 

oooooo 

oo 

»oeo 

£8 

oooo    • 

MOOOOOXCOiOOOOWaoON        05000        HrtHrtHHNNNHOHt>NrtN«MNO)INNNNNHNNO( 

lOOOOnOOOH  Ot-H0005  Ot-HtH-H  i-I  t-H  t-H  i-H  t-H  ,-1  T-H  ,-H  H  1-H  i-H  ,-H  O  i-H  T-H  T-H  t-H  ^H  i-H  O  H  1-H  H  i-(  H  i-H  T-H  T-H  H< 


N*ON©iOiflOiONO>000)10 
MtDWl'OOlH'VtOlHOCHHN 
■^iT*(-Qi-<jiir5-qiTfq<lOCO''*'CO-*J"J,>0 

O  O  <M  CO 

hoo>o> 

■^"*  CO  CO 

NOOOO»NOCO»Mnf300C<5INtONOMOO?3<*00!OONNMH®MNCO 
OOOOOOOOOOOOOOt^t^000500(Mt^OOOOt^cOt^Ot^t^-OOt^r^OOl^t^050500 

cocococococococococococo^cocococococo-^cococococoeococoeocoeo 

NOCS00      'iO®iO<0  0>NiOOCD      • 

H«                     •  t-H                 lO          OJ          t-H 

NK3      •  lO 
t-Ht-h      -00 

CO  i-H  CO  r~ -<Ji  00  05  00  »0  00  00  CO  00  CO  lO  CN  t-i  iO  t-h  Oi  CO      •  00  i-H  CO  CO  CM  O  CO  CO  t-H 

1-H  I-H  <N  T-l  T-H  i-H  r-l           <M                  CM  I-H  CN  I-H  T-H  CO  <M  T-H  <N  T-H        •  CO  Tt<  T-H  CO  CO  ««  CN  1-H  t-H 

OOiOMTTOOiQOiOOHOOOOfflcO 
OiNNOiu-JOXOH^cotOOOtl* 
0005000005050005000000000000 

OONO 

CO  IO  Tt»   TJ 

ooooooob 

TCtOiOU5  05K5  0>0  0  tNffiOOOONOOHOHNOOONMHPSVlOOCN 
rfifrfiTj<lO-^,'9iiOlO'OI^lOO5lOlO-V^riC0lO00CO»OCO'^lCO'*lC0C0lOlOlO 

ooooooooooc/;ocooocoooooooooooooooooooooooooooooooooooooooooooo 

rH<M 

a  a 
o  o 


I  CO  "*  CO  t-H  CM  • 


5  § 

a  I  sill 

'  "",3  3 

o  o 

P3P3 


#tf 


3, 
'2. 3  !q  , 
ooo 
PhCS-SI 


d   ' 

3 

c 

0 

05 

>- 

H 

g 

oiXio 

r: 

»H 

o-c 

0 

.s.s 

,Q,Q 

O  O 

Ph  pi  a.,  tf  co  P5    :Ph     Pi 


MhC|)th 

flfiflf) 
OOOO 
w  co  w  ai 

3  s  3  3 


IP-PhPh 


:phPh 


lO  ifj  lO  lO  I 


(ONNONCO     05 


CO    NOOlOh    00    MNcNinvocoaiooooco 
r~-    oot^cct^co    t—    M  «  X  C  «  C  O  ifl  ic  w  to 


Cl'-Hco 

6  o  o-1 


lO- 


fc     £ 


>>      >>      >>        WV'O'^ 

•c    ■£    t:     tj  g  g  >: 


"£.3.3  © 


o  o  o  o  o  o  o 

©  QJ  ©  QJ  ©   ID  *D      r-     p       •» 


t-h     NU3MNH     CO     CO  00  i-H  CM  f^  CO  CO  «« 

6    6  6  6  6  6    6 


o  o 
o  6  o  o  o  oo  o  o^^* 
fcfcfcfcfcfcTZ.fcfcsfa 


£  £££££  £  £££££££££66 


SB      SB 

3  3, 

,3         ,3 


s  s  a 


.2.2.2.2.2.2.2-0-0    £ 

,3  ,3  ,3  ,C  ,3  ,£  ,3  ©  ©     g 
OOOOOOOPhPh   o 


+J  J  3  3  3 
f^  (^  ^  ^  o3 

©  ©pqpQPQ 

©  ©  as  ©  © 

OOPhPhPh 


.to-d' 

•   C3    C3 

.-O-O' 

:wwc 


•d  "O  -o 

WWW 


dd 

WW 


£  5  c3 
OPhPhI 

O         t-H      OCOVlOtO      t^      00  05  0 


i  c3  csiSid 
(PmPhOO 


hNm^iocom 


TH       T-H   T-l  T-H  T-H   T-H       tH       tWt-HINIM<N 


CNtNC^(Mc5(M 


254 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq— tpnpojd  rei^iui 


laaj— Lttdepieioj, 


■;aaj— iWdapno 


£83  bb 


£-§■§•§  ££ 

55  :  :  :oo 


■^  cN 

00  00 


03-^JO> 

s-§a" 


CM  >Q  CO  t^  00  <M 


I 


;a9J—  QWB\d 

ran^Bp  a  AoqB  apr^i^y 


188J— I8A9] 

■B8S    Avopq   epnmjy 


pe^j^uod  ssaujpiqj, 


•^aaj— doq  otj  q^daa 


3   O    ©    C3   PI 


u 


o3 
e8  O 


2!z 
co 


iOOiOO! 


C3  1-H  CO  < 
^H  CM  CN  I 


NMt        HfflOlHi 


I  00  CO  lO  CM  00  ' 


oooor^oor^t^oot^ 
cocococococococo 


liHTtl  t—  CO  O  < 


tji  -qi  tjh  cc  oo  tr  »o      co 


OCCO00NO 


<  00  t^  O  00  O  CN  CO 


ONO        t~-  CO  O  O  t-- 

C>  CN  CN         COlOCO^fCO 
oooo       00  00  00  00  00 


NOOMiOOOiOM 


PI  PI  H   fl 

o  o  o  o 

CO  CO  CO  co 

S  S.S.S 
2222° 

O  O  O  CCJ 


pi  g 

o  o 


OOOOOOOO     O     O00     t- 


■*mNcoiNh>c»h 

"ddooddod'-* 

d  £  £  £  £  £  £  £  &  d 


»o     -cf  CO  CN 


O      O 


o  o 


■^COtNi-H 

666dH'   «   M°    ° 
£  £  £  £  d    d    d<5  ^ 


pfcfcfc£fcb££p     a 
dmmpqpQpqpQpocQO    p 


flflrtfl 

o  o  o  o—    _, 
co  co  co  co^    3< 


-fc    fc    fctf    OT- 


W  ^W^£££o  o  od  d 


tJOWjbXJ  W) 

tS3    CO    tS)    N 

C 

B 

p^p^pEHpCH 

* 

■= 

^t3  ^  i^ 

n  K 

p  PI  PI  PI 

o  o  o 

o  - 

s- 

c 
c 

c3  03  c3  03 

;  coco  co    ;    ;    ;    ;_co  k 

2 '£'£'£  2  2  2  2 'He 
2  o  o  o2222  °  «- 

* 

c 

'd'd'Oooooc 
o  o  o  ,53,2.2.5  2 

C 

2 

2  2 
22 

c 

3 

c 

2 

o§SSoooo££ 

s 

^ 

P^^pqpqpqpQC 

C 

oc 

c 

o 

a  th  m  «  tp  io  co  n  oo  a 

— 

cmw*  locoNcoa 

c 

CN 

co 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


255 


1 

X 

- 

c 

c 
c 

(- 
- 

1 
1 

o- 

- 

I 

N- 

1 

a 

V 

0: 

0 

t- 
a 

r 

- 

- 

1 

' 

:£ 

!   © 

-«2 
!o 

.00 

©    ~© 

sag 

IP 

© 

CM 

00 

c3 
C3 

Oil    from    conglomerate . 

Quit  in  sand 

Gas,  938  feet 

Saltwater 

Gas,  920  feet 

Gas,  938  feet 

— 

t- 

c 
c 

c 

c 

C 

C 

«2    ■ 

1  | 

-  !  a. 

cu  "O  >— 

"ci  ° « 

«»  fcsg 

a 

O 

*JI 

s 

SS 

S§ 

|£2   >> 

ft 

i 

00  010 

> 

n 

08 

CM 

CO 

!0 

00 

1 

10 

OS 

8    ! 

OS       OS 

c 

OS 

-*l 

CM 

00 

00 
CO 
OS 

OS  OS 

1- 
00 

10  CM 

CO  00 

oc  00 

lo  »  m  t>.  "3  h  <ir       r--  lo  t^  re — 1  .-1       Os  OS  t-  i~  01  -i-  f-  i-       i.o  x>  OS  i~  cc  co 

i—l  O  CO  O  i-3  CO  O         LO  O  O  M  M  O         C«c;C]i'.   -■:          i-Ci'^NS 
t-h  OS  O  O  O  O  O        OOIOhOOI        i-h^hOi-h^hO^hO        OOOOt-hO 

O  Tf« 
>-H  OS 

rt  rt  N  N  e  0  ro  [-  h  N  CO 
l^COIN-rcNcOCTNli-ICOCNt^ 

U1  N  N  M  lO  O)  '-D         CiJiflM^OOi         i-Hi-ICOeOOOCOCOCO         C<NrHCONN 

W  CO  CD  ®  Tt<  ffl  CO         ■*  0  t  O  O  O         CO  Ofj  CO  CO  t^  'V  UO  •*         -*fi  OS  -<»<  -}<  t^  CO 

co  10  ■*  ■*  ■«<  •<!<  ■*      •*  10  -*  co  •*  *o      co  co  Tt<  co  co  tf  co  ■<*<      rf  ->*i  -ti  -*p  CO  'V 

CO  10 

OS0500CO^t<Oi-ICOOSOO-^!       • 

CM  CO  t-  m  tr~  ^  r-  0C  CO  t^  CN      ■ 

CO  CO  ■<*"  ■*  CO  Tf  CO  CO  CO  CO  ■<*'       • 

0 

Tfl 

CM 

OSO 

CO 

CO 

CO  "f  i-H  ■* 

00  ^H 

lO  00  00  <N  CO  CO  t-i  00  <M  10  O      • 

COCMt-lCM          lOrHCOlOH        • 

-H  CM  CM  CO  CO  t^  O         MflOlOOOO         NHCOMNO'*'*         COOiONt-tN 
^  ffi  IN  U0  O  IN  H         i-H  t^  CO  CO  ^t>  O0         CNt^<NOlOCN-'*CO         CO  l» -H  W  t  H 

00  0  os  0  os  os  0      osososooosos      00  00  os  00  00  os  00  os      o)o>o>c»c»0) 

00 

OS  TP 
00O 

oo»coTi<oocooot>o    • 

CM  CO  CO -^  CO  CO  iO  CO  >0  CO  OS      • 

00  00  00  os  00  os  00  00  00  00  00    • 

0 

— 

— 

1 

■s 

— 
PS 

re 

5 

c 
PS 

1 

M 

c 
p 
IE 

c 

PS 

co 

= 
0 

V 

p 
IE 

- 

K 

c 
0 

— 
0 
pi 

CO 

PI 

c 

05 

x 

c 

PS 

i 
c 

P 

IE 

c 

PS 

c- 

i 
c 
0 

IE 

c 
pS 

P 

0 

| 

IE 

0 
PS 

CO 

i 
c 

OS 
P 

IE 

c 

Pi 

c 

£ 

IE 

c 

PS 

> 

c- 

a 

1 

i 
— 

c 

CC 

§ 

C 

IE: 
c 
PS 

:  p 

,  c 

K 

>.£ 

h  0 

QQP3 

CO 

1 

r 

IE 

0 
PS 

p 

c 
•/■ 

IS 
c 

Pn 

co 

PI 

c 

I 

IE 

0 

PS 

c 

•fl 

i 
0 
t/I 

p 

1 

PS 

CO 

i 
8 

IE 

0 
PS 

CO 

§ 
p 

c 
PS 

P 

0 

c 

2 

CO 

i 
c 

c/" 
P 

IE 

c 

P 

c 

P 

IE 

0 

y 
P 

IS 
0 

- 

> 

a 

a. 

1 
I 

'- 

c 
PS 

!co 

:  p 

=1 

"Z   0 

1 

— 
c 

PS 

CO 

g 

p 

1 

PS 

i 

•r 

p 

c 
PS 

c 

c 
— 

c 

p 

i 

i 

- 

! 

IC  CO  ' 


O       CO  ^H  ^H 


NNClfflCOiH 


CO  1-H 


o  o  o k  J    "    " 
^Z^o    6    6 

03  t»  en  ^    'H    'H 


^    ^ 


©  o>  o  >j    >->    >> 


«-/  C      V,  V. 


OOOPQ   H   pa       tf   P3     P? 


c 
55  c§ 


I      ■*  CO  Ifi  CO  1-H  i-l 

h    wra CM1-1 

-•_:-:  0000000. 

ts  •d'd  ©    ®©©®©3>>>i 

•53  *53-s  ^i  mxxxmXv    © 

c§  cc=a  S    SSSSSfl^  -^ 

©     ©  ©  *     ^  *  *  *  ^^r4  o     o 

03     03  03 hrf 


6        O'O'OOO^-; 


h-3    ^ 


©^  ©^^^pTpT 
o     o  o  o  - 

03      03  c3  C3 


>1L 


o  o  c^    o    o 

IS  15  3  o  13  IS 

OCOCi  o  C 


o 

w 

Pi 

si 

O   PQ 


2  2 
IS  IS 


o  00 


o 

;o 

O      O  O  O  O  O  w 

0    oooood 
P3   rtp4p4«p^O 

o     o  000  OQ^ 

tJO     W)  "5)  Ml  "S)  "So  w  o3 

rt    g  a  pj  a  g^w 
'?   E  fc  e  p  P-i_ 

CC3       CCOCCOCCOOCjCom© 

M  WWWWWPhPh 


O     ^      CM  CO  rt<  iO  CO  i-H  CM     <M 


03  pQpqpapq  S3  3 
►r   ©  ©  ©  ©c^ 

lO       CCNOOOOrH 


1« 


256 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


03  ^S 


■siQiieq — pnpojd  rei^ni 


•198J— qidop  pnOJ, 


ss 


•}oaj— q^dop  no 


t3 

.l-H 

+-> 

o 

I 


o 

El 

8 

o 
?»» 

rO 
O 


xnn^p  eAoq^  gprvji^y 


■WOlXI^OO-HiOOOtONrtt-OlOtONlOlONIMNMOlOlOOMCinOCINrH 
MOi»^00>MH(X)FH'JiiOiOO-t<O^COlOCO-*HCO'WINtC(N(C©CCC 
>— iOOO>-ii— i>-ii-<Oi— lOOi-ti-HOi-HOi— (Oi-hOOOOi— lOr-tOOCO 


•}98J— ]8A8J 


!0OMlOOiOt000HXlOt'0aiOffil0(0'*tDlO00«'CNC<5NC0OMM 

WTti^^cccococOTt<co^TtioocOTt<co'n<coTtico'ti-*|-^-*coTi<eo^M<'^Tti 


•}99J— 

pg^BJigugd  ssan^oiqj. 


COMrHlNlN 


•198j— doq.  oi  qidaa; 


tfiOiOr-lOOlOHOOOt^OwOOMINOOlONOiavXr-lOOlOtOMK'OtQrt 


S  9  9 

o  o  o 


c3,0  C3  ' 


:## 


as 
11 


NmNMi 


l  CO  i-H  CO  ••*  CO 


.9 .9 .9 .9 .9 .9 .9 .9 .9 .9 


T^  CO  rH  CO  "H  CO 

a  a  a  a  a  a 
o  o  o  o  o  o 

w  in  m  to  [O  K 

o  pi  a  a  a  c 


o  es  J3  ',5  !S  ',5  2  5  2  "jo  5!5°5 15  5 15  '5  2  ° 

•O  j-  OOOOOOOOO  0*0  O  O  O  O  O  CO 

:^«pi5Pip3PirtP5p5tfp3  :p3tftfp3p5P5  : 


rt  IN  CO         T 


o  o  o 

£££ 
a  ri  a 

CD   05   CD 
X)  TJ  ^ 

o  o  o 
999 


£   £ 


o       o  o 


J    J 


>»>>  o  O 

O  O  .-  - 

C3  c3  ^  'd 

"-"-•  O  o 


o  o 

fc  52; 

PI  c 

o  o 

pa  pa 


C8  O 
2^ 


2  2  2 

3  3  3 
coo 


,*>  M  M    M 

co  co  co     co 

.2    .2.2  ^  ^  I  ^ 

^      ^c]  ^     c3  ^  ^    rt 

O    00  £  s  ss 


OOO)     o 


cn    co 


1  * 


BLATCHLET] 


TABLES    OF    WELL    DATA. 


257 


i 

EC 

X 

3 

c 

' 

B 
cr 

0 

f 

to 
>a 

CO 

03 

a 

CO 

as  S 

S3 

is 

a: 

1 

05 

c 

s 

— 

O 
>0 

| 

o 
o 

3 

1 

o 
•a 

1 

1 

12 

ss 

>ooo 

o 
o 

3 

5 

O  CO 
05  05 

g 

— 

os 

8 

o 

PC 

c- 

8 

05 

05 

o 

!  - 

c- 

— 

C  C 

cs  5 

>0 

35 

(Mt^t^i0ii0>O«5Ot-lf0^C^i0O00OTfiC0i0C<)'«ti( 


iNNiOMNOOOiOOnNHVOOOiONO^tOMl 


iOC5^HOOi 


iO^HO^HOi-iO-HOT-iO-HOi-HOi-iO^-iO^HOO»-<0^-iO^-iOr-iO^HOi-HO^HOOOi-iOOOOO 


eo^iOM^^ec^MTrMTriM^cOTtiM^eo^w^eo^evsTrwTP-vevsrriMT^ccTfico^co^ 


tptoor  ic  -r  z  rrorciOLOio 

(50050000505000500050005 


"fOOOOCT 


NTtiOtONOiOONWN' 


00O500O500O500O500O500O500O500O5O50OO500O50OO500O5COO50OO500O5O5O500O5O5C5O5O5 


o      o      o      o 
5?    53    53    53 


53  55  53 


P2    PQ    CQ      PQ 


6 

6 

6 

c 

6 

6 

ea 

6 

d 

if 

g 

g 

<D 

M 

-• 

•w 

<N 

lO 

CO 

t 

53 

6' 

to 

53 
aT 

5Z 

53 

13 

53 
© 

53 

to 

9 

CO 

13 

CO 

CO 

CO 

o 
53 

o 
53 

o 
53 

O 

53 

o 
53 

o 

53 

o 
53 

'a 

2 

£ 

s 

X 

A 

3 

3 

A 

c 

o 

o 

o 

c 

c 

o 

Uj 

CO 

EC 

CQ 

01 

CD 

CO 

CC 

CO 

•y 

•d 

«4 

•d 

>. 

&■ 

1 

>> 

03 

03 

O 

o 

O 

o 

O 

O 

o 

o 

O 

o 

o 

o 

O 

fen 

Eh 

Eh 

feH 

H 

H 

H 

"3  3  "3    "3    "5 

,0    A    A      A      A 


1/3  CO 

"3    "3 


-3     .cj 


a 

* 

5^ 

£ 

a 

s 

a 

a 

s 

B 

£ 

a 

s 

a 

£ 

a 

s 

s 

g 

a 

a 

a 

o 

C 

O 

rr 

'0 

■-o 

t- 

00 

_ 

N 

-n- 

'0 

t>. 

00 

^J 

w 

rri 

t» 

on 

c 

s 

—17  G 


258 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spireq— jonpoid  psiirai 


•J88j— to  dap  p^o  j, 


laaj— q^dap  po 


■M 

c 
O 

i 


O 

o 


188J— arrejd 
uinicp  aAoqc  apnipjv 


•}88J— J8A8[ 

•Gas   A\ojaq   apn^i^v 


•}88J— 

paiBj^auad  ssau^ojqj, 


•?aaj— do}  o;  q^dsa 


a  <»  i   i    I 


a^a   a~3 


§3 


©  cd  t-  ©  cd.cb 


N»*V 


O5  00O5  00   ^00OiCT> 


OOOOojOOO 


£c» 


•-hi-hOO        O       iONO)HO*^HNNHOlJOOOO)H©OHroO>' 

lOOOO  O  t-C  O  *H  ©  i-H  ©  r^  O  r-l©,-i©rH©^,-<©©Oi.-l©1 


CO  ^  ^"  ^3*  ^        "^ 


CO-*FCW<CQ-Q<m-&COi}<CO-&CO-f<C0tt-*f 


o  co  Tt<  co  •* 


00     •  kO  t~-  ©  t--  >o  <tf  CO  < 


'OCjOSD 


iOhNN        CO        OOHNCO'flONOOOOXf  OOOONhOOOOO! 

i  ^-i  cn  -.o  cnj      ^h      u}cpt«ii5Scqw>0(Qciine4NN  oo  go  ^«cii--rtacc 

i  o  OS  ©  ©  ©   oc  ©  oo  ©  oo  ©  oo©  oo©  oo  ©  oo  ©  oo  oo©  ©  ©  oo©  oo  © 


JO        ,  CO  H  CO  H  CO  H  CO  I-H  CO  i-H  CO  ryl  .  CO  -^"O  ^  ( 

_   oooooooooooo  oooo 

coco        co              co        cocococococococococococo  co  co  co  co 

as     S     >,S  >  3.S.2.S.S.S.S.S.S.9.2.S  :.S.S.S.S. 

cS,3  e8A. 


OQPS 


o  o  o 


©      t~-  t—      ©      O  I 


s-T    tS 

o    o 


55      55 


H    Ol1*    w    oon      to 
6    do    6    do      6 
Z     55     55  5555  55  55^     fc 


©  ©     ©     cp  a> 

CO    CO       CO       CO    CO 

"IB© 


E^cHEh^       SSS^aSSSSSS 


I  5 


03  O 


8* 


3 

A 

A 

jd 

fl 

A 

fl 

A 

.O^ 

A 

.Oxl 

jq 

A 

o 

O 

c 

PQ 

o 

o 

O 

O 

O 

OO 

0 

OO 

O 

O 

O 

,_, 

oj 

S3 

,_, 

,_, 

CN 

lO 

cot^ 

00 

»o 

rH 

CN 

CO 

<N 

N 

[525 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


259 


miotoanaioMMi/iiDKoioi 

.9  .9  B  B  .9  B  B  B  B  B  B  B  B 

3  3  3  3  3  3  3  3  3  3  3  3  3 

OOOOOOOOOOOOO' 


a  a 

o  o 

co  co 

a  1=1 


—I  CM  .CprHCM 

as  :  s rt  fl 

O  O  .  O  O  O 

CO    CO  CO    CO    CO 

pi  pi  :  pi  G  a 


:«    Ph« 


■  9 
>3  o 


03O.O  0,0,0,0  O 
-     o  CO  O  O  OTJ 


CMCO- 

Pl   PI 

o  o 

9  9 
33" 
o  o 


9  9 

33 
c  o 


a  pi 

o  o 

CO    CO 

9  9 

33 

o  o 


:«  :  :« 


.CM 

:  pi 


:k 


© 

•s 

■-I 

fit 

>> 

i 

> 

c3 
OS 

o 

8 

o 

§ 

1 

<mJ 

CM*" 

3 

as 

o 

©      • 

"el    : 

£  : 
+*  *. 
•a  : 

co   ; 

©   ! 

«2   • 

iO  © 

CO  .© 

-OS 
COlO 

CJCi 

35 

i 

1" 

SQ 

as 

ga 

o 

©   © 

t-l  lO 

C  -f 

CT><35 

as"" 

g 

«£ 

CM 

a 

o 

ii  ! 
j-S  : 

•1  : 
Li 

'd  ©  ; 

pi,2  . 

£o 

i 

SB 

CO 

ft 

a 

CM  CM  CM 

o 

IC 

low 

uO 

a 

o 

rin 

o 
CO 

o 

CM 

aa 

I 

CO 
9> 

1 

o 

CM-<S< 

r- 

I 

33 

o»oa 

—  X 

OOMMMCOrtNNTfiHOfflOCqM 
TfiO-^iOCOcOCOLOTfiiOCM-^CMCOt^ 

OrtNNTriONOMCOOtM 
H"OTf(NO^OCSNiO(NCDCD 
r-lOO-Hi-H'-lT-lOOO^HOO 

H  O  CO  CO  iO  i.O  M  »  ffl  O  t^  N  H  rt  (N  U5 
CCiflMHHOOiONVOOHOOCO 

OOOrHO—H-HOOOrt— IHHrtO 

e 

o 

lOMN 

©oo» 

lO'fiO'OicOMCD'WOmoOiOCOCDN 

rtOWCCCDiOMONNOCDN 

oo-*iot^c35ioa5'— i  cm  -<c"  oo  co  co 

Oi  i— ITf^iOiONCN'J'iOCOOCOJOlCCiO 
.-<rrcOCC00O5OiTf<CMiOO5Oi00aiO>CO 
^  ^  ^  CO  ^  CO  CO  ^f  ^  ^  CO  CO  CO  CO  CO  ^ 

CO 

m  t^-eo 

OlOH 

t»<  rji  io 

•     .     .     •     .     .     .     .     .     •  CM  -"Ji  -*>  CO  CO 
\    '.    '.    '.    '.    ',    '.    '.    '.    '.  ""' "" ' M  ,"H 

t^OiCM      -CO      •      'NOOW'*'* 
Tfi  CM  i-H       -CO      •      ■  CO  i-H  i-t  rH  i-l  CM 

•O       'WiONCOOOCOOOWHN      •      • 
•  CM       .         t*HZ         HHrtNNMN      •      • 

CM 

-*CM  • 
CM 

iflOOOiCOOiOiOOOOOOlOCOIN 
•V^OTtnOCOOM^MtOrONCOCNI 

ooo50ocjc»o>cx)050oa5cjooiooooo5 

NiOOOlONiONNCNNOOiO 
N^C0CD0)-^00O<NTt<NCNC<5 
CX)O5O300CXDC»C»C33O5O500a>O5 

OOOCOCO^COlOONOOlCONOSCDQO 
-H^cO000000Oi-<J<i-HTt<00CT>00a>C>CO 
O5C35O500O50000asO5O5CX)0000C»00C5> 

S! 

o 

CM  TtiO 

PI  Pi  PI 

o  o  o 

CO  CO  CO 

Pi  a  a 


P3P5P5 


C>     I>OiOi 


CO      (NWOOOOOCO 


I  I 


ooo      ooooo 
fc  Jz;  £    £  ££££ 


5?    »     E    5?    Z 


T3      T3 

"o     "o 


OOOOO 


fc  »  5? 

tT  j-T  (-T 

S  I  I 

®  o  » 

J  ^  J 


o    ooo 


s  saa    a 

Q)      Q)  O  D         CD 


^    5Z5  jz; 


a   a 


a 


^2  ^2  ^2 

,0  ^2  X2 

<^  <{  <J 

«3  -a  «a 

a  pi  pi 


O      O  O  O  O 


o  o 


a   a  a  pi  a  >  > 


O      O      w 

fc   53   » 


a   a   a 
000 

«  ^  ^ 

Eh      B      E^ 


111 

CO      CS      C3 

B    «   B 

"d  tJ  *d 
©  «  © 
Ph    Ph   PS 


00        f-i     CM     CO 


1  111 

P5  BfQffl 

©  ©  ©  © 

Ph  tfPJ.g 

rt<  lOCON 


s  a  a 


000 

3  3  3 


o    000000 

3  333333 
o  000000 


o  o 

3      3 
0      0 


CO     I>-  00  Ol  O  i-<  CN        CO 


4  * 


260 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•s^JiBq— pnpojd  XB]%ui 


•ijeaj— TUdep  pnoji 


•J88j— q^dep  no 


CO 

8 

S 

g 

o 

^. 

o 


o 

o 

I 


•^99j — Qwe\d 
ratuBp  8AoqB  gpn^jy 


•189J— I8A8I 

■bqs   A\oj9q   apn^rnv 


'}99J— 

pa^j^ongd  ssgu^oiqj, 


199J— do;  o;  q;d9Q[ 


p  S—  £  £  ® 
co  .2?  »  >  .2  «£ 


S£ 


8 

'WO      • 

il«  : 

•.do1" 

;d<3,£ 

cs-C  o 

:  g  >>.g 

!sli 

'd  >»- 

8 

8 

FH 

Q 

o 

c 

s 

8 

§ 

§ 

8 

§ 

g 

1 

i 

c 

s 

OCT 

/■  - 

o>  CO 

00  OS 

c 

5 

OK 
CO  --H 
00  C 

8S 

poos 

CT> 

r-l  ,_,  ,-1  ,-H  ,-H  O  I 


I  O  i-H  1-H  «H  O 


15? 


'OOlt^OOOiOOOi 


»-*NhhNO( 
OHOOHCBlflOMlOOOIMlOaiMtD 

coeoM<i*Tj<cC'q<rt<cofO'*coco^tico 


o>cooocoooi-Hr-oocNc©oot^e>$ 

COCOCOCOCOTjioOCOTticOCOOOT* 


i-H      'NO 
CM      n-H<N 


CO        0)"OOHff.iOOCOiOOC(NiOO)MtD 
Oi        O0O0O5OiO5O0O5Oi0O00CT>0OC»O500 


OONNOOOOiOOMOmW 

fflinotoooHtoooiNtooot^ci 

OOOOOOOOOOOSCOOOOSOOOOOOO 


CO  *H        ,i-HCN-<J< 

p.  p  :  p  >H  pi 

o  o    .  o  o  o 

CO  CO       '    CO    CO    CO 

.a  .3^a.a.a 

,Q  42  03,Q.Q,O 

O  O  Jh  o  o  o 

P3  tfcopHpSpH 


qqP3 


a     p  pi     pi  pi 
o      o  o      o  o 

CO  CO    CO  CO    CO 

,0.   03,0,0  03,0,0   =3 
O.J-  O  0£  O  0£ 

Ph  to  Ph  Ph  co  Ph  Ph  to 


o  o 

CO  CO 


.S  >-..9.S  tA.S.S 


O  O  £*  O  O  >3  CO  o 

P5otPhcoPhPhccPhPh«5Ph    :ph 


o 
£   o" 


s- 

"   6 

6 

6 

6 

6 

6 

6 

6 

o 

6 

es* 

%   V- 

£ 

fc 

fe 

tz; 

fe 

5? 

ft 

^ 

^ 

£ 

o3        cS 

d 

,d 

■d. 

d 

d 

d 

d 

d 

d 

d 

A 

fe- 

h 

O 

o 

.Pi 

H 

.a 

.i3 

.a 

ci 

C3 

pa 

CQ 

pa 

pa 

pa 

pa 

pa 

pa 

pa 

pa 

pa 

^J 

• 

^j 

^j 

^j 

^j 

^j 

* 

_^ 

^j 

^ 

a 

C3 

03 

03 

03 

03 

03 

03 

03 

03 

03 

P 

CD 

CD 

CD 

H 

H 

H 

H 

Eh 

Eh 

H 

H 

H 

Eh 

H 

=3 

4 

<<j 

=3 

4 

=3 

«a 

4 

4 

°3 

4 

-d 

d 

«d 

-o 

•d 

•O 

»d 

•d 

>d 

■d 

•d 

Fh 

(H 

o 

o 

o 

o 

o 

o 

o 

o 

o 

o 

«2 

* 

£ 

£ 

is 

Ee 

^ 

^ 

1 

* 

^ 

ft 

03 

03 

03 

c3 

03 

03 

C3 

03 

03 

03 

eS 

Lh 

Fh 

U 

U 

O 

O 

o 

o 

O 

O 

O 

o 

u 

- 

~ 

•< 

-. 

~ 

- 

_  •« 

•> 

« 

•< 

•« 

c 

c 

03 

03 

03 

03 

03 

03 

03 

,c 

Id 

CD 

2 

CD 

?, 

CD 

£ 

£ 

CD 

e 

£ 

s 

C 

C 

fen 

Eh 

Eh 

EH 

Eh 

Eh 

H 

H 

H 

fe- 

H 

BLATCHLET] 


TABLES    OF    WELL    DATA. 


261 


+3 

£ 

OS 

a 

O 
g 

i-T 

0 

09 

5 

CO 

4J  4j       . 
05  0    ^ 

a"  a* 

4- 
V 

•r 
C 

|| 
woo 

a  a 

CO 

ffi 

«£ 

1 

GO 

a 
a 

c 

s 

c 

' 

1 

s 
a 

o 

§ 

o 
5 

o 

o 

i 

o 

o 

Q 

co  tn 
ft 

«N      ft 

§ 

oo 

G 

1 

o 
8 

CO 

3 

1 

?5 

CO 

5> 

1 

03 

11 

82 

05  0 

3 

a> 

3 

C5 

1 

OCOMCOO)NO)ONiO(ONTl<0©HH^Ni00100tOIN01^Nt>.u:^0000(NtON»OOOOf"OOOOTtilONNlOi 
O0QH!0CC00Ht^OO0HDNONOHH«OroMN00MNH(0H'<)irt0)lO00ff.M(SlO©0CaiNN«OO©00a( 
^HO-HOl-HO>-lOrH^HOOO-HO^Hl-t^H^H^OOrHO.-lO-HOl-lO-HOOOOO>OOOOOOOOOOJOOO< 


ON 

N.« 

co^r 

«rHOOCOO)0)OMINiON0500»«0>0«NHtOMOOMOO'OaiOiO 
CO  V  CO  **  CO  CO  V  V  V  CO  V  CO  CO  CO  CO  CO  V  V  CO  V  CO  ^J1  CO  V  CO  V  CO  V  ■* 

00  * 

^o 

»0  T»1  Tt> 

o 

Tf< 

-r 
= 
■* 

-1 

OCNOiOCOCOiOUO 

MCOCOOIOHOH 

•  CO 

•  fflMOOaOOOOOOOKOiOOOOHHNNWiONH 
•HMCMNNiOiOHMN        CO  CO  •*  V  rH  CO  CN  CO  i-H  CS 

rtW        CO 

•  «o 

CO      • 

00  CO 

co-* 

•tNlOO 
•COOOi-H 

£ 

us 

Si 

ss^s*0?0'?? 

CO  COO  O 

00  0  00  05 

ONrtOMMO'<f'*<00'WlOiO«)lOtDNO'a> 
5OH00COO>©O5(N0>'*INO)00C0«DO)CDiONt-i 

00O100O3000000O50000OJ000000000000O100OJ 

OONNOOONOJ© 
COOiOONMCOOON 

ooooooajooosoooool 

CN  CN 

8S 

ooots 

1 

05 

<N 

a 

§ 

941 
943 
1,001 
1,100 
907 
917 
912 
922 

f~  t~-  o  -f  00  ( 

t>.  00  t^-  00  00  < 


m    ujio    in 


o      o 
55     55 


<-H  .-I      C^CO      i-H      1-H      O*      VON      ,-H 

6      dddddddddd 
55     £  5555  5?  £  fc  555555  fc 


«      «    0)       « 


b         Ui        t<    Ih    I. 

c>    <d    o?  cp  cd 

=3    ^    3S3 


55  Z^^Z  fc     55 


§  98  a  a  9  99s  9  9  a  a  a  £££g||f5£   g 

w  ww  w  pa  w  www  pC    pC    Ph'    pC    Ph'    i-i  hi^WWWh,'  ^    W 


o    o   •    o 

55  55,g  55 

9    9  *  9 


K  WpC  W 


*r   *r   m 


Eh    fr«    ri 


^2     ,QX!    _.      O      O      O  O  O     ^ 

^  ^^  p>j  o  o  OOQ 


r«  ^)  ^5 

CO  CQ  CO 

4J         -fa         +J 

S       S       3 

III 


■a -a 

c3     c3 


•d  •« 


_o  o  o_o_o    o      o 


CN     CNCMci     N       (S       N       «       « 


o  OO    o 

«  s^s'^iSic)  '^    '^    3  33  3 

tf  tfooooo  OOP  oo  o 

—I     NMV050N     00        --1        CN  CO*     io 


o      o 

3    3 
o    o 


262 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


•spjiBq— ^onpojd  p^rai 


•^8j— mdep  IB}0  J, 


o 

:fl 

>  « 


oo 


•%9&l— mdep  UO 


o 
O 

CO 


^88j— aireid 
tiraTBp  aAoqe  opn^jv 


•}aaj— 18A8] 


poiBxjatrad  ssaujpiqj, 


00  iO  (M 
NtDN 
-HO© 

■*00Tf00P5t^^l<0C|iCNTt<t0c0tOC0NOlOOt^C0t0mtD'-l!O 
*-H©.-l©.-l©T-H©,-l©,-l©,-HOr-l©.-l©r-H©.-H©,-l©rHO 

NCON 
CO-*<T»< 

OOlC'^tOMOOMM'Offli-IMtDrtrOiOlOHlNi-INCONffiTfM 
lOi-iiO-H^OtNiOi— iiOC3iOCOCOCO«O<MO5Tt<O5CNlcOCO©CO0CCO 

co^eo^co^coTt<co^co^co-fl"co,'J-coTr'co'*cO"<J,cOTf'eo-'3« 

388 

<N  (N  r-l  (N  TH  CO  »H  (N  TP  rt  Ttl  T-H  CSl  <N  ^  <N  CN  CO          -J1TJ1CO       -iH       •  CN| 

KDNNtMOCMlOlOrtOONlOrtO- 


•^eaj— do}  <n  qidaa 


r-KNlM 

2)33 

o  o  o 

phpsph 


CSX! 


oooooooooooooooooo 


C3,Q 

co  Ph  co  Ph  Ph  Ph  co  Ph 


jrj  oi  c3  fl 
02 ,2  a?  >  .2 


u 


OOOOOOOOOOOOOOOOOO 

tftftftfpipjtftfpjtftftftfpjpitftfpj 


Ph    • 
C3  O 

as 


t;  o 

CO 


N 

0 

o 

o 

o 

o 

o 

O 

O 

o 

o 

o 

O 
7< 

o 

o 

0 

fe 

fc 

£ 

fc 

B 

» 

ia 

fe 

£ 

P 

9 

® 

<B 

<X> 

g 

(gj 

as 

3 

s 

s 

m 

o 

tp 

_ffl 

.ft 

."3 

,H 

.= 

IS 

72 

n 

72 

:t2 

n2 

— 1 

>H 

t2 

xl 

CO 

XI 

CO 

Xl 

CO 

CO 

XI 

CO 

•x) 

CO 

a 

3 

S 

a 

a 

S 

g 

2 

a 

Its* 

1-9 

>-i 

1-9 

1-9 

l-i 

w 

^ 

H 

w 

^ 

w 

Ph 

Ph 

Ph 

d 

03 

PS 

rfl 

C3 

,* 

^ 

d 

ri 

03 

03 

JM 

id 

w 

4d 

^ 

q 

r^ 

M 

,M 

en 

K> 

■si 

3 

£ 

ri 

S 

x 

Ph 

pq 

c 

o 

d 

3 

s 

a 

XI 

.2 

4 

XI 

ri 

ri 

-rl 

Ti 

T) 

5 

5 

XI 

03 

xi 

sa 

OS 

PS 

XI 

Xl 

3 

3 

o 

M 

S 

a 

a 

Pi 

PCS 

PS 

O 

c 

0 

M 

s 

a 

<M 

CO 

o 

co 

i~ 

00 

09 

o 

CI 

co 

lO 

H 

1^ 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


263 


s- 

9 
« 

"r 
QG 

"c 

1 

C 
— 

9 

B! 
i 
-o 
P 

cv 

►J 

"3 

■s, 

9 

s 

CD 

1 

i 

30 

8 

0 

1 

'3 

0? 

co 

a 
3? 

1 

00 
09 

1 

ft 

i 

1 

CD 

«£ 

M 
OS 

CO 

c3 

- 

CD  — 

O 

.-- 

— 

co 

c3 

O 

i 

i 

5; 

a 

■  - 

3 

CN 

o 

■I 

1 

oo  o 

«3  -«i  CO 

3 
§ 

§ 

s 

8 

x 

OS 

CO 

OS 

CO 

3S 

00 

o     • 

OS       • 

o 

OS 

i 

OS 

00 

SO 

- 

CO 

— 

OS 

ac 

OS 

c 

re 

oa 

CO  CN  CN  tO 
Tf  t^  TT  CO 
OS  0C  OS  OS 

OS 

00  CM  CD  tj«  O  i-  so  t~  os  0:  co  co  ~-  OS  CO  CO  .-i  CO  CN  < 


■OOOOO 


CDOO-a'CO-HOt^t^^H^t^ 


'fflt^COOX! 


1  CO  ^  CO  ^3*  ^  -^  tji  • 


CN  CN  lq  — i  O  CO  t>.      'Hi 


'<Ot»OMMiONW       •  Tfi  CN  < 
'CN  CNi-HCO^H  CN       -CMi-K 


i— i*t-oo5^-W«eSi-t-*eocNTH«ocMcoe«cooB 

IOSXO300OSOSXOSXOSOSXOS0S   X  OS  OS  X  00  00 


csoioococoocsoor- 

f?  bP  !>;  O  CN  O  OS  CO  — 


lOt-rexip-r  x  xoxoiooooocN 
•  -  w  »-.  s_  w- -■-  ~w  w-  w  ni •  ^<)  t  co  M  —  r)  N  rj  cn  so  —  i~  co  co  t~  -»  in  co 

X  O  OS  X  X  X  x  os  X  OS  x  os  X  OS  OS  X  OS  OS  OS  X  03  X  OS  OS  OS  OS  OS  OS 


.3  3 
33 
o  o 


a  a 

as 

>v3.3 

c3.c^ 
•s  o  o 


=  ro 

o  c 

°9    3 


r-HCNCO 

3  3  a 

O  O  Q 


rHCO^—ICO" 


i.0  32.0- 

i  o  o  o 


3  «  a  3 

o  o  o  o 

co  co  co  co 

3  3  3  3 
3333 

o  o  o  o 


is  o  o 


ICN-^CO      .CN 


,  CO  i-i  CO  CN  CO  • 


3  d 
o  o 
2  "3 


rHcNi-icoco-^eocNco 


3  >>3  3  >*S  3  3  3  3  3  >>5  :  •  SSSSSSS's's 
c#i"J3 222  'r?-2  rf'2 2  m& 22222  r>-2±>±>  222222222 
iooooio^ooiooooooio'ti'Cooooooooo 


OS      0C  CO      CD         lO         00 


00      X  X     00 


00     OS     00 


«        X 

a 

c 

CN 

o 


^    Z 


c      c 


l  CN     rr         rt 


cu   pj 


C3  C3 


£  £    £ 


c3        C3 


c    o  o    o 

c    a  g    c 

a  aa  a 


Z     ^  fc  ^ 


s   a  a  a 


3         =3 

3 

2 

3 

9 

3 

3 
^5 

3 

3     3 

,3    ,3 

C3 

c3 

C3 

03 

C3 

C3 

03 

03      C3 

a  a 

s 

§ 

S 

S 

§ 

§ 

£ 

S     a 

CO  CO 

"3        3 


— <  CN 


C^      S 


o    o  o    o 

3  33  3 
o  oo  o 


,3    ^3    A 
O   O   O 


264 


OIL  MELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sjaxiBq— pnpcud  reprai 


•;aaj— q^dap  ibioj, 


•;88j— q^dep  no 


3 

« 


umjep  aAoqe  apn^iqv 


188J— \QAQ\ 


pa^Jieuad  ssaujtoxqj, 


•^89j— doj  oj  q^daci 


U 


oooooooo 


000(000010 
CO  CO  CO  ■*  Tf  M  rn  N 
OCiOiC5C>CJiCJiOO 


OCX3<N^C0cNCi^c0t^C5Tt<00L0O»aT^rHT}<0i'0'<tii-H00i-l00C0i0""Cf<»Cit^-e0 
(OiOiOiOiONtOHiOH^!OCDNNHt»iONecNtOMiONt^(DcDN(DiOH 
OOOOOOOi-HO»-iOOO>-iOi-HOOi-iOr-iO^HO»-iOOOi-iOO»H 


ONCOtO^OOHCO^COi-lcOINiOOiOOJCHCrHOCailMOltNNlOlOiOMN 

^TPTjiTt<^c>icocx:^oou3cocor^cooocN^t^cor^coccT*ii^<Ncocor^.co''cr'oo 


o©ioc<ioooNtN<o    •  >o  co  eooooi  10  coo  co  oo  o    'coth    •og>i< 
mco^MNniccMM    •  co  ■*»<  co  co  cn  co  t  i-i  oi      »-i    .cococo    'conn 

N^OO<0  0»0)NMH!ONNNNHHt^NiCHOO>NOCOCOHtNHMN 

CN(NTT'5<CS|FHCSC0tN(0C0rHrHl0iH©rHC0'0iH10iH'>l.(N<0OCNtNC0INNN 
050305050SOiC»OOOC»05050i00030005C>0005000JCJ00100050505000>OiOO 

CO     !     !      !     I  CM      I  ^H  CO  1-1  CO  CN      li-tNrtNcOi-iNHtNiHMi-iNM      IhNMi-i 

i  ■  i !  • ;§  i§gggg  igggggggggggggg  -iiii 

.§  :  :  :  :|  :.IJl.i.i  rJilJJJJJJJJJJJJ  :jlll 
3  °  °  °  °  2  ©22222  °  2  2  2  2  2  2  2  2  2  2  2  2  22  °  2  2  2  2 

o'd'O'd'd  ox)  o  o  o  o  CO  ooooooooooooo  o"0  o  o  o  o 

^^^^^                v_„_^_„^        v-,, u ^-^-^^                *-^S 

t^  (N  eq  rf<  cN»  CM  t>. 

00  00  OS  CT>  00  00  CO 


00  00     00     oo  oo 


ffl   ffl 


c-i  co  io  -»<  rH  ■«<  co    oo  t-    cnio    oj  co    ■<}<    co  h  cn  co   cn  cm    eo    eo-f 

HHNNr-IHCN 

oo'"o'o°  oooo  ooo  o  o  oooooo 

*7  'Z  !7 17  S''  17  *7  hZ    £h  Z    /5    Z  £<  7\  7\    ZZ    Z    Z55 

aaaaaaav  *>    ®  ®    *>  a?    <u    <d  a>  a>  «    <do    «    «« 

rtrtgcfldfl^  M    MM    M  M    M    M  M  M  M    MM    M    MM 

c3c3c3c3§§c3S  2    22    S  2    2    2  .2  .2  .2  .2.2  .2  .2.2 

333^333  rt  "tf  tf'tf  tf  tf  tf  tf  tf  tf  tf  tftf  tf  P3P3 

:  I  i  !  :  I  :    :  :    :  j    :  :    !    i  :  4  :    \4  4   14 

:•::::::  ::::  :::  :  §  :  £  *  §  -5  « 

::::::::  :    :  :    :  :    :    :  :  «  :  3pq  «  Sb 

OOOOOOOO  OOOO  222  2  »rt  2     ^ -a"     T3     ^"O 

2222322  3  2  23  3  3  3  3  3  »  3  ,*»  «  ►?» 

OOOOOOO   O  OOOO  OOO  O  tf  Q^tftf^tf 

^SSSSSS  2  ^22§  S  cl  S  <S  8  8  £8  8  83 


g  . 

02 


BLATCHLBY] 


TABLES    OF    WELL   DATA. 


265 


e3  co  e3  o3  to  3  c3 

o     OO     OO 


o 


00  00  00  00 


OOOO 


oniooooo 

ooooooooo 

c/T  c/T  r/~  (/T  (/T  c/T 
03  03  03  03  03  03 

ooecoo 


O        "OO 


•nNNo 

•  oiooio 

•00  00  oo  o 


cOOtO 
NHO) 
00O  00 


O  O  1-H  h  CN  O 
00  00  O  O  O  00 


)00MiO<N0)'*©0CO«0>0tOO'- iTfiTfi 
>ir5OTJ<r^lO00(NCNC0r^C0<Nc000I>.OC 
>0000000.-hOOOO— <000< 


io      r~  co 

i  00        t—  00 

iO      oo 


N*'*'*aiNiON«30CONcO'fl"HlOO>>ON'*<*e<30)lOM 
^050NCONaO!OOCB®WOi»WOiNNNO)CDOi!DIN 
OOi-iOOi-HOO'-ir-iOOi-HOOOOOOOOOOOO 


.-IfONNlOCOHCO'fNO'J'lOfOanOtDW 
00C0'D«'>»'O'0Mr}irHNN'<}'(NC0NNTHlNOO 

82 

gs 

CO'*t'COCOi-HeOiOCO»aO''9<OOr--COOiO-HiOOQCDOr~.-HiOOO 
lOOOCN-nr^OOOOOOCOO  — ihONNNOWOMN 

oo^co^-^cO'>»l'^|cc,<»<'<si^j<coTt<'<ti-^iT)i'VTrTrT}i'^'Tf<'<»i'9< 

SSSSSS  IS  ;8338  :  :?338§S 

%  i 

CN  'OmomiOM  •  •  -t^OOCN  •  -OINO  •  •  •  -O^H 
CO      HOIOIO*'*^      •      •      '"^        -V      •      •i-HCCPO      •      •      •      -CN-* 

ITS  00  "O  r^  iO  CO  00  <-H  iO  CO  t~  iO  CN  CN  .-(  00  C^  CS  C^  <N        T  O        OO        N»OOt^OOMOO'*MO)00'*»'*OOHHVONCCH 
CO  -H  (N  CN  00  CO  O  CN  00  Tt<  *»<  r-H  O  O  T*  CO  00  O  O0  00         00  00         O00         Nl^iOOOatOONNtOCCNNfflOOOtOMOlHCDNOOHffl 

00005010003000005000000000000000      cooo      oooo      ooooooooooooooooooooooooooooooooooooooooooooo 


1-H  CO 

s  3 

o  o 


CO      ,CM  CO  CN  CO  CN  ' 


ico< 
o  o 


a  a  a  3 


,3,3,3  0^j2^1^ 

O  O  CO  oooo 


.3.3 
o  o 


,3,3 

o  o 

titi 


,3  ,3  ,3  ,3  ,3  ©  ,3 
OOOO  CO  O' 

{SPSPhPhPh    :pc? 


.1  :JJ 


,3  0       fl£  o^ii  oo  o  oo  o  o 
CO      £  o*©1  o  O 'O O "3 t3 *0 "3 "3 

prj  :    cart  :phK  ::::'.!'. 


ss  :§a 


03".3.3 

tjoo'O^o'O'O'oo 
ggPhPh    '.PhPh    '.    IPhPh 


oSSqS 


O  O  O 

PhPhPh 


i  iO  00  00     O       O        iO 


"Oh-        t-  CO 


8  SI 


O     O  O  O  o     o       o 


S  I  S  B 

3 

£ 

£ 

•*-*  9  9 

o 

o 

o 

.2.2  3  3 

£ 

£ 

PS 

tfpsmm 

pq 

cq 

O      O      O  O      O  O  Tji 

£  fc  5?  £  £;z;d 

a"  a^  a~  a"  a"a^. 

o    o    o  o    o  o  C 


pqpqpQ     eQpqpq'cc!     cafe 


o  o 


M  O 

O     (H 

.d  ® 

©33 

Q2C0 


CO  CN  r-i  CO  IO  TJi 

d  o  d  do  6"3«)Ni 


iOCNtt     i-l 


O  O  O      O 


CN     00< 

J5r5r5<(AHf2;od66    6    do    o    do  'drT'd  tT 

rlz;  £  £  &  £  ££  £  £  £  ©  ©  ©  © 

„,.   _   ..      „      „  „      ..      _c3(3cd  <S 

M  d  d  d  d   d   d  d   d   ag©©©  © 

^  '©■©'©'©'© '©§§§§   §   §  §   §   §  §  cs  call  « 

35  ££££££ssss  gggs  ss£££  £ 


n 


ts 


«     k^  w  «  O)      o> 


.-h-    1-5 


©     a.  ©  G 
©    a>  «  © 


**? 

H 

£s 

Fl 

^  3 

3 

.d'0 

■d 

fe  fl 

G 

O  fl> 

£« 

P3 

oo    o    ooooo 


©  00000^^,3,3    A    &A    A    ,3,3,3,3,3    A 

SSSSS^oooo  o  oo  o  ooooo  o 


<N      CO  T  ^H  CN      CO 


iO    co    t^ 


icn?5c^c5^c5<n    c5    <m  S    co    coco'-'      M 


266 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq— ^onpoad  xei%ui 


laoj— mdop  p3io  x 


oooo 


'881 


•}98j— q^dap  no 


CO  •  CO  CO  CO  f-  00  CO  •"»!  CD  CO  >0  < 
i-H  'NHHOOOtDfOlOi 
Ci      •  OS  O  OJ  Oi  Oi  00  OS  OS  00  Oi  c 


© 

o 


uiti^Bp  QAoqe  apnqq  y 


Or-HOi-HO^HOOOOOl-HOO. 


OOMWWHMOQNO)' 
iO^HOO^HOOOOOOi 


■jaej \dAQ\ 


pa^neuad  ssaujpxqj, 


188;— do;  o;  q^daci 


ONOOOOOCONONtOCeOOOONONOOQOlflOlMOOMCOlO'V 

'*INC000N0»C0WOH0)©'«'a)Hrt(DHO00N'*0!NOi0 

Tfico^co^eo^^TtiTt'^co^Trico'cri-'tico^'fl'CO^'V't'ioco-^' 

Tt>  ->r  as 

r}i  tP  Tf 

•      '      •  <M  00      •  Oi  *-r  OO TPOOOWiO      ■  CO  O  O  >0 

...       CO      .  <M  CN  tN ,_i  i-i  tj<  i-h           •       t-i  CO  C< 

;eot^ 

oor»owoTro>NCNn*trt^oN<Da:oooioonNo 

NHtSHDOOOHOOOlOffitDTtiOOOOiOOail^HnOOHO)^ 

<j>ooo>ooo5ooa>ai05oooiooa>oiooo>oooaiooooojo>ojooo 

88S 

ooSSo 

Cq        ,NrHlNrH(NP5       .  rH        ,HP)CC> 

&  :  a  a  «  a  p)  i  :«  :  &  i  £  £  :  ;  :  &  :  :  a  a  a  a 

o    .oooooo      o    !  o  o  o  o        ,    .  o    ,    .oooo 

2  03  33^333  o'B  ,33333  ©  ©  ?3^£  ce3333 


3    3  3  3 
o      o  o  o 


u 


o    o 


o    oooooo 


ca  ca     cm  qatccacGtcca 

C5      0?         O      ©  4)  O  O  4)  CD 

•a  3  -a  ^■§i'" 


o    oooo 


£  55 


£  £  £  ££££££  rt  tftftftf  a  a 


£* 


02 


o  o 

o  o 


oooo 

3  13 3 3 2 19 3  3  3333 
o  oooooo  o  oooo 


oooooo 

3  3  3  3  3  3 


1 

| 

I 

a 

c3 

a 

C3 

pq 

pq 

n 

pq 

>d 

nd 

13 

•g 

cp 

a> 

P4 

P4 

P4 

« 

t~-      00  01OH«C<3 


lO  CO  I—  00      Oi 


BUA.TCHLEY] 


TABLES    OF    WELL    DATA. 


267 


e 

X 

' 

c 
i. 

- 

g 

3 

' 

09 

o 

o 

I 

1 

CO 

CO 

§ 

I 

s 

00 

of 

09 

C; 

O 
00 

8 

o 

u 

CD 

03 

08 

* 

[fl 

I! 

si 
o 

1 

00 

i 

o 
ua 

o 

o 

i 

o 

e 

i 

o 

o 

ON 

o 
3 

r»> 

s- 
P 

CM        O 

CO 

OS 

U9 

OS 

lO 

OS 
OS 

so 

C3 

CO 
1  - 
OS 

OS 

-r 

as 

l- 

OS 

1 

0 

- 

3 

X 

X 

ir 
x 

rx 

CN 

llO-^NlOM'OiOlO^OKJNTjicOi 
OTffflHtDNOCOiHi0^050NNCOtiONI^COOOCO(»CONlONHNrtlOrHO'*(Olftl3)CONNN^(NaiNI 
iOr-iO^HO-HOOi-iOOOi-i<-iO^HOi-<OfHOTHOi-iOT-iOi-iOi-iO»HOFHOOOOT-HOOOSi-iOi-H< 


CO  00  rH  rfi  CT>  < 


ICO        f  MCOHIMHtOHiOi 


'MTfOOOOONHNOIMOtO' 


iNONOeiOM^OONNiOrtOOO        OS 
lOCiOtOOJiOHCOHMHlNNfiinOOOHTtNlOOOCW        CO 

ooo>(»a5ooo5»05<»0503c»oso5ooooooosooooooosoocoooo5cco5oco5cooocoajcy)o;cco50>ooo>ooo  oo 


,  CO  i-H  CO 

0  «  a 
o  o  o 

c«  5  3  3 

£  o  o  o 


aaasa  :sa  :g 


08.0,0 

cqPhPh 


.0,0,0 
o  o  o' 


■S'-S 


i  CN  i-H  CN  rH  CN i  rH  CN  rH  CN  t-h  CN      I  CN  rH  CN  rH  CO  rH  CO      ;  CO*      !  rH  CO      !  1-4 

oooooo  .ooooooo  ,o  !oo  '  o 

"23     ,  co  en-  co  en  en  co  en     (  en     t  w  w     #  en 


O  PI  s 

o  o  o 

CO  en  en 

Pi  PI  PI 


<■&'£ 

o  o 

iphPh 


333 


p  ^— >  \->  \~>  w 

fa  3  3  3 


a  rii^ij  :.|^fl 


233333  cs3333333  c?3  ©33  es'3  °3  co3  os3  ° 

000000^0000000^0'000_(-0,00'30J30'0 


3  O  CC  OT3  OOOOOOOOOOO  O  £  OOOOOO  O  j-J  Cd  O  O  J3  0^3  O  _J-4  O^  0*0        *-< 

^■"CTlOOOOOOSTtiCOiri 

t^-t^-t^-      r—      »^      eo      t>»    co      co 


iv.eol>,t-,r^t^i^.      t~- 


t--       i>       CO 


O      O      O  O' 

55  55  ^^ 


i-H  CN  rH 


55        55        55        5? 


6  pi  A  0  A 

-z  ,o  ,a  ,0,0 -h~  ^r 

^  o  o  oo-s  -3 

t-T    -e  S5  <g'  ®i2-^  -^ 

PI     PI  g  +2  £££  .2 


■55  &    55    £    55    £ 


55     55     55     55     55 


CN        CO        <*■ 


O 

CD    £ 


p-T     O      O 

«     55     r5 


55     55     55     £ 


P         CO         W         fP         W^rl     hH^S      S         S 


s   s   a   s   a   §   a 


+j     a>     cd 
5^  a!   ra 


m     zo     m  M     W 


C3        C3        C3        ri    f<        • 
M      M      M      M     Q       ; 


w     c3 


a    a    a    S 


:  :**  ^ 
•    :  '.&  g 

w  .2  sii  ^ 

C3      t)     Jj     xijj   C3      C3 

S  tf  o  ooa  a 

(O     N     M     OOH     IN 


X      M      M  X 

<n         CO         CO  w 

rd          .0          A  A 

c3  c3 


-^       a 


S    S    a    a    a 


CN        CN 


rC  Ct3  fc 

C3  CP  CD 

a  a  a 

CN  rl  CN 


"d  i3  rt  /d  ! 

c  o  o  o  J  0" 

so  sb  ct=i  to  .2  .2 

CD  CD  CD  CD  ,3  & 

a  a  a  a  o  o 


cc 


UO 


268 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq— ^onpoad  reiirai 


•%&}— q^dap  pnoj, 


•}88j— q^dep  UO 


■%qq} — auejd 
um:rBp  8Aoq«  epn^piv 


•^91— J8A9J 

B8S   Avopq   epmpxv 


•}99J— 

pe^j^uad  ssgujpiqj, 


•}99j— do*  o;  q^daa 


&§UaA- 


S£ 


<2«2 

.-HIM 

OOOO 

a"  a" 

Salt  water,  946  feet 

Salt  water,  950  reet 

Salt  water,  954  feet 

Salt  water.  950  feet 

.3 

i 

c 

s- 
«l 

1 

IS 

oooo 

OMOH 

— .p        CO 

o 
o 

g 

S 

t-i  t- 
OiO» 

oc 

OC 

3 

we 

0>0 

CO 
C3 

OC  CO  CN 

ojoo- 

o  "C 

5>a 

esost^ 

HOff 

ojoooc 

oooo 
oooo 

)iONN»0><OOHNCOO(OiOiOtrtCOH( 
iMHNHCeONONMiOCJifiMtOKOmi 
i^i^H^f-iOOO^HOOOOOOOOOOi 


COCOCOCOCO^^lO'^'CO'^*^**'^^'^^*1'^1' 


VOO>ONO«©HOO)(NNNNlOO«M)0  O  <-H  -H  <N  O  t*  ^h  ^H  »-H 
i-H  CS  -<r  CO  -<*i  I—  CO  Oi  t~-  O  CO  <M  Tt<  CM  CO  O  CT>  O  »H  t~  O  O  Ol  rH  Oi  Oi  <M  O0  00 
00  00  00  00  00  00  O  00  00  OJ  C5  0>  Ol  Oi  Oi  Oi  00  Oi  Oi  Oi         03  00  00  05  00  00  00  00  00 


<  CM  i-H  CM  CO 

;  C3  sb  sa  ej  da  el 

,  o  o  o  o  o  o 


£  sb  fl 
o  o  o 


c3  O 


3-d  o  o  o  o  o  ot'O'd'C  o  o  ot)  O      O  O'O  O  Old 


,       *wJ       W       ^       ^       W       W  ,  ,  ,  .WWW 

<saass§ : : :  :aaa 


03  £>£ 


OiO 


t^t-lO     00     o 

K5WO     CO     CO 


'"*'  CO  CO  rft  lO 

60666    6    6 


$$ggg  1  g 

WWooo o o 


<DN    N     CO 


CMtHi-hcoOOOO^, 

66  6  o^^^    - 

..•.-.-ooooX 
ooogoOOO^ 

OOOOhhhhPJ 


000 


o  o 

££ 
>^ 

a)  03 


o    o 


Q  Q 


222   2 
EHc-iEh   EH 

££*■    fc 


000  o  o 


c3    ^     +2     -Sti-S 


"Z  '3  03  4)  03      03      03 


03  03  03  03 

'd'O' 'O  d 

©©©'S'S'g'g'P' 
S^S'S'©  000 
000  O  «r-  TT  V 
OOOO  &  £  £  £ 

°3°o<3  =32222 

mk^OOOO 
03030303     „_..., 

N    SI   N    N+J-P-U-P 

03  C3  O 


03030303^bt-iUi^d 

&h  ^  ^  fe  Eh  E-t  Eh  Eh  O 


03   03  03 

EHEh  EH 

c3«3  <3 

fa  b  b 

00  o 

03  03  a>     g  g     g 

EHEH  EH   PQW   M 


I  <N  CO     •"»<     »0 


NOOOOHNCO' 


TJ  o 


BLATCHLET] 


TABLES    OF    WELL    DATA. 


269 


o»  goc  oo  £ 

co.2  co  cr"if 
€8*0  03  03^3 

O     OOcc 


O  OS  O  O  O^ 


lONNOl         CO 


lOOtDNNiOMNO 
■  CD  00  CO  CT  ID  CD  CO  CO 
lOOOr-HOOO^H^OOOOr-iOOOOOOCNOOOO 


CN  -H  00  lO  00  lO  •*!  Tf<  a>  05  Oi  O  OO  CO  !>■  Tf  lO  00 
WOOCONCOT  OCOTiOf  CNOOt^lOlO-^-CN 
OOOOOOOOOOO       »iOOOOOO 


1  co  ^f  ^*  ^cf  co  ^r*  ^f  ' 


CO  CO  CO  lO  CO  i 


•*   "*  "f  •>*<  CN   ■*!  Tf   ■ 


CNCDCN 

HHM 
Tfl   -<3<   Ttl 


ONn'MffliON 


eOH00tC'WNOMNNOM0i0iOONi.0(N00NOh-CSON 


i—l        IOCON 


ICNt^CNlOCDCOCSOOCN         MtDOCOHLON 


—I        .CNr-HCOCN 


CS.O 

is  ° 

coPh 


>J 


S£ 


:  n 

,  c 

CO 

:  I 
,2  2 

"0  o 

:p3 


q  q 
o  o 

CO    CO 

q  q 
S3; 

o  o 


q   •  >>a.s 

Q  O  08^,00 

otl  £  o  od 

s  IosPhPh  : 


:  q 
■o  o 


"-  c 
OS  £ 


:^P3 


:  o  q 
=^3 

.oqPh 


tf  :« 


q    ;  fi  fi  a  b  fl  pi    ;iq 
o      oooooo      oo 

,1  :.S.H.S.sJ.S  :|.§ 
3  °  3  S  3  3  3  3  °  3  3 

o'd  o  o  o  o  o  od  o  o 

pj  :tfp;pitftfpj  :p^pg 


S.9  :s 
3Iq  °3 

O  CO  o 

tfpH  :ph 


"q  oVj 

o-do 


O     NOO    ffl 


I"-      t~-    t> 


Tf  CO         CO  CO  • 


i-(        V     lO 


55  55 


O      O      O  o 

55  55  55£ 


55     55  fc     55 


g    g  o    §    8.3 

q  Ph  i-;  h,"o 


oo  co  o>  «o>-|W) 

o  d  6  ^^,3 

£55  55  £*£ 

oT   oJ"     aT       of     oT  03"*  os"  "d  'd  "d 

|S     m       m        [ot      33  !S  OOO 

03     03        03           c3        O3o3o3  ... 

OOP        O      OO  O  ^^k> 


o    o 

55  .15    cocN'cmco.-i 


o  o  o 


,cf  3"   o  6  o  6  o 

oo      ~  ~  ~  -  -   o 

q  q  fq^SSS  "d 
^  °*  ,q,q,c!,q,q  ® 
Ph   Ph   uimuimxn  Q 


o     O  O     ~      JJ.-? 

-7-    h7-h?-q3     qSiqa 


15     55   5555 


o    o  o+f     if 


05  ©  03 

-q^^i 

ooo 


o  o  o  » 

5555  5555 


•d  -d 

05      03 

P  0 


03      . 

QW 


q  aqo 

tJ  ^J  ,_t   0)   03   C3   © 

H  H  H  P-i  P^  Ph  Q 


SSS^^.-«. 


2   £ 


-d  *d 

o  o 

*  £ 

03  03^ 

^    ^w  o  o§ 

03          03       (13      -        -  -pq 

9          9       9«      =3  03^ 

2     S    H£    2  £© 

P2       PQ    pQH    tH  E-tPn 


03  03 

Ph  Ph 

t3  -d 

03  03 

Ph  Ph 

CO  t^ 


cHHEh 
■d'd'd 

Ih  ki  h 

o  o  o 

§§   §  ooo 
PQP5  P5  *a-*r*r 

'g'g  "S   £££ 

O  -H       CN       CO  -*i  lO 

(NCN     CN     <M  COCM 


pp 

PP 

_0  03   03   03   03   03  O 

3  q  s  q  q  d  3 

Q  PhPhPhPhPh  Q 

CM  CO'VlOCON  00 


ooo 

3  333 

O   OOO 


.q  ,q  .s  .q -q  .q  t3 
.q.q.q.q  03,q  o3 
OOOOPhOPh 


O  ^H  CN        W*iOi 


J  15 


270 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sjaxreq — ;onpojd  psprai 


•j89j— q;dap  pnoj, 


•^88j— md9pi]o 


CD 

.2 

o 
O 

I 
,gi 

«0 

s 

g 

o 

c 

I 


ran^Bp  8AoqB  apniTjjy 


■B9S    JiO[8q    apn;i:qy 


•199J— 

pajBuauad  ssaujpiqj, 


•^89j— do;  0}  qidaa 


3  Si  o3  fl"g 
oq.2  ®  >.2<£ 


ooooooo< 


CN  O  -*  < 


'  CO  i-O  lO  >o  lO  CO  00 


iNooootOTroanoNOJOooNCioajinoO'fl'CuD 


aio^ccoioNt-r-itoNMai'fl'O 


o  a.  >o  ■«•  eo  o  io 


335281 


•sl** 


•  end  +f 

■  os  oo -g 

•  O     to 


S8    £> 
P 


OOOO       OiOH 


HOiO        OlOC 


NNHtOOIMNOfflCONNHWNNiOOOONNVOlXWNN        NN® 
<M  TMO  •*•  CO  O  CO  CO  CN  CO  in  :■-  to  K  I  5  N  I  ".    ~   JO  O  r^  O  rH  CO  CO  CO  00  00        ©  CO  2; 

ooiooc  r-  r.  r.  ~.  ~  ~  ~.  r--  cr-  ©  05  cs  o  o  k  o  »  o  c;  x  x  »  oo      o  oo  oo 


1=1  0. 
O  O 
CQ   CO 


iCNeocMeo    ;  cm  co  cm  co  cm  co  cm  co —i  eo  cm  cm  eo -h 


aassas  iasscaassaaaaaa  la 


>  o'0  o 


o  £  o 

TJ  OX? 

:ps  : 


CO  CO  CO  CC  CO  CO 


MHO  i-H 


58  55  $ 


r^oi  oo  ci  t-  h    cp 


(M     i-i 

6    d 


co 


rl      CM 

6    6^. 


ooooooo      o   ^ 


o      o      o 

fc   £   £ 


^r  «    a      c      pi 

1 1 1  i  i 

i    T3    t3      **=!      ^ 


QOQQQO   O     DBB 


o  o  o  _•  ~  £  £  ©  © 

£  £  £  "3  ^  -a  s^^ 

3    .9  .5  .5  £  £  .a  .a  >>>> 

>     >  >  s  :=j  .t?  ^  _22.ci 

"eS       «  «  «    k  k!                 J2i2 


P  ■  ■  -1 

03  03     ■ 

pqp:    ■ 

-o  t-j  .2 .2 .2  t3  -2    .2  .2  .2 

a]  ©222  ©  2    2  2  2 

tftfooog  OOOO 


OOOO 


&6 


r*  o 

CO 


•OCOt^OOOiO      ^H         CM 


-H         CM      .-H      CM 


s  a  a  fi    :    :  :Jj,2 

«      »      «      ©        .        .  -0,0, 

8  8  8   8  .2  .2  .2  eg 

*  £  £  £  £  5  5§3 

o  o  o  o  o  ooo 

t^OCi-HCMCO  •*»<  lO  CO 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


271 


£  \f 


Is! 


t3  o> 
Si* 


Zoo     O 


^  :s 


££ 


03  d- 


£  :^ 


S3  to  Q 


Si  e§  073  3  o  £ 


o  o 

53  53 


IS 

3 


'O  OOOO 


Pfi        Q 


QPe 


■  OiOOOH 
■010)00 


K5NH       •  IC 


Old 
CO  CO 
05  00 


IH  —I  CO 


iT(f*M»!OOONrt*M'<fNN 


OOO  OO! 


'  rr  CO  ■*  •"*!  *cr  iO 


10  -f  »o  10 


-*<  00  T  CO  CN  OC       'ONT)<H(Ng)00l 
HrtHrtHCO      •  CO  <N  CO  <N  <N  CN        ( 


CO  >o 

ssss 


r-O 

CN  « 

CT>0 


lOOONt^NHOOOOOCOMHOOOOO 


OS  00  00 


g 

c  "0 

P3   : 


CO  -f         CO  CO  CN  CO  CN 


aa 


aaa 


>  O         o 
id         O 

:  :    « 


.0,0 

o  o 


~  o 

XX 


<0OOOOO,q,qO 

:  :  :  :  :  :xx  : 


aa 
11 


o  o 


H  p| 

O  O 
w   CO 


tftf 


COi-H 

c  o 

CO    CO 

.2.3  i» 

,0,0  C3 
O  O  >- 


co  co  m  00  > 

CO  CO  CD  CO  < 


00        CD  00  00  CM  i 


00     CD  CO  iO  rfiiO  CO  Tfi  CN  CN  "tfi  • 


CNCRO 
NCDN 

rn  ^a<  tji 


1  CD  CD     CD     CO  CO  CD  CD 


i-H        CN 


lO 


COCO  CN- 


OOOO 

000000  oz  >z  *z     Z  5z  666066 

-.9  .5  .5  .5  .9  ~  -  -  -  ~  - 

'"ft  'ft  'ft  'ft  'ft  r$  M  M  M  J%  M 


10-^rHcNcoco    ^    cNMcD-no"*1^'050 


O,-.      ,_J 


,0  ,0  ,0  ,C  ,0  .O  ,0  .    ■ 
ft  ft  ft  ft  ft  ft  ft  o 

S333SS3o 

5S5SSSSSSS 


O   C    O   O   O   O       fl 

*6  *6  'O'  'O'  r6  'o*     t5 

a)  0)  03  03  03  03      S 


66666<->ooo^r 

o  o  o  o  o  >, 


CO    CO    CO    CO    CO 

.2.9.9.S.2 
S  3  £  3  3 


£03 


_,  t3  d  'O  T5  >,  o 
03030303030303030353(2 

ft  ft  ft  ft  ft  Q  Q  flfloo 


go? 

a** 

111 

_rt   O^5 

oaoQ 


OOOO 


OOOO 


£££   {?   ££££ 


pqpQwwpnpqm 

^   03   CP^   03^   03 

,0.0.0,0,0,0,0 

ftftft  ft  ft  ftft 
SSSSSSE-2 

c3  c3  c3  c3  c3  c3  03-^ 

0000000O 


■~   ct  ct  ci  ct  ct  o 

pq  pq  pq  pq  M  pq  .g 

'O'ti'O'O'd'd  fc< 

03    03   03   03    03   03  O 

P4tfpr5p4««  5^ 


N  00  Ol  O  rH  CN  WV 


£1  fl  PI  PI  fl 
OOOOO 
CO    CO    CO    CO    CO 

'£  B  E  'S  '£  2  2  S I  2  2  2 


c 

■§.ss 

pi^° 


o  o  jj 

!d3  pi 

OOP 

^HCNCO 


pq  pqpqpq 

'O  "O  t3  'O  •■-< 

03  03   03    03^3 

P4  tfpijpgO 

■^  lO  CO  t^  00 


00  O)  O  .-H  CN  CO  tt  lO  CD  i-H  CM         ^H         .-HCNCC 


lad 


272 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq— lonpoad  \vi%ui 


•^aj— ifldep  i^^o  x 


•J99J— ttadep  no 


CO 


ran^p  aAoqe  aprupjy 


■88S   Avcqaq   epn;i;tv 


pa^iiongd  ssaujprqjj 


•WQ\— doi  o^  qidaci 


%K 


T3  § 

a 

la 


oo    -oooo      oo 


CO  <N  05 


«<tcom«iHO(Ciotoooo      >o  ■«<  est  •** 

fflrtOHMOCMfflrtXiOrt        (Nt-iOOO 

I  ,-1  r-l  —I  ©  rH  O  .-»  ©  1-H  l-l  r-l,-l,-H© 


£S3! 


VTf  -v      co  Tji  co  •v  co  ■*•*  co  -<r  co  -v  ■*  co  oo  eo  eo 


ootoNimNaofion-NO 

©00©00©i-ll-eOOOi-lTt<a5 
CO  Tji  CO  CO 


coco  co-* 


©oo      jg    .©r^r~oo< 


r^t^kC^ 


©CO         WNMXNMXXiOafNCOTClOtDMiOOlNHKJW        CO  CO  HO 
00  ©        00  ©  00  ©  00  00  ©  00  ©  00  ©  0000  00  00  00  ©  00©  00  ©  0000        oooooo 


UNhmhNw- 


o  o  o  o  o  o  o 


i-i      .i-iCN 


ooo      oooooooooco      ooo    .ooooooo  o    .oo 

s!!Jj   JjjjJjjjJJj  :1J|  :.IJJI.S.sl  .§>.§J 

'r>  °r>  )q  °,q  )q  )o  )q  O  Vj  |q  |q  O  °^q  ]q  J2  )o  |q  \o  ,Q  ,Q  c3"io  )o 

OOOOO'O'OOO'O'OOOOOOO  o»-oo 


,0,0.0 

ooo 


.OO 

o  o 


c  c 


2 
ja  o 

C    0 


00     N     N 


oo        oo      oo 


^f<        CO     (N 


fH       r-l       ©       t- 


3   £ 


o    o    o    o    o 
£  5?  £  £  £ 


o    o    o    o    o 


£  fc 


o      o 
5?    £ 


£  £    £    ££££££££ 


ft  :Q 


,3      ^    ^Jfl    X    fl 
£       &     ts     £     £     £ 


35  o£o3 

c3  d  -t-3     a  -^  0  -^ 
fe.  o  <o     o«)o« 


a   V,  a  a  a  ^ 

tji         ifl     tC     N     00     O) 


03      03      03         03         08 'jr.   B      fe  C'b  H 

§  §  S    9    S1& I&I& 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


273 


"c: 
0 

z 

c 
c 

c 
t 
I 

(" 
c 

- 
o 

£c 

c 

'1 

o 

Tj 
pi 

C3 

s 

c/T 
C3 

© 

1 

CD           CD 

cd      «£ 

£  s 

CO        CO 

t/T       c/T 

C8        03 
tuO       to 

T           T 

"o3      *e3 

A      A 
to     m 

s 

CO 

m 

03 

cm 

CP*~ 

A 

m 

Salt  water,  885  feet 

Shale  gas,  650  feet 

Shale  gas,  670  feet 

Shale  gas,  625  feet 

c 

3 

ft  « 

c 
c 

o 

LO 

o 

LO 

£ 

»o 

§  I 

CO 
OS 

o      io 

00         00 
C3          00 

CO 

05 

CO 
00 
00 

1 

00 
CN 

o 

05 

CO          05 
T         CO 
05          OS 

g 

00 

CN         CO         <N 

CO        CO        t- 

00         00         00 

CN 

T           O 

o     o 

OS 

o 
o 

CO           LO 

CN        t^ 

OS          05 

1,144 

1,088 
1,063 
1,149 
1,110 
1,023 

1,157 

1,062 

1,131 

1,165 

1,080 
1,153 
1,111 
1,062 

00  OO 

LOCO 

CO         CO         GO         COLO         CSO         lO  CO         T         i—i  LO         NC         CO 
CM         CN         i-i         CO  t—         TCt^         HN         !>.         TOO         CM  CO         .-I 
_          ,_          _          ,_io          TO          T-lO          O          .-HO          HO          i-l 

©NNHOt-         COCO         C5         lOONGCC 
WHMlOOiN         T  CO         CO         CO  CN  T  00  CO 
CO  T  T  CO  CO  T        cot        CO        CO  T  CO  CO  T 

CNCN 

T  CO 

coco 

t~-      t      cn      t  m      ho      lo  r-      co      o  *o      ooo      r- 

t*         t-         00         CO  CN         IC  CO         00  CN         CN         0OH         f~  T         GO 
CO         CO         CO         CO  T         CO  T         CO  T         T         CO  T         CO  T         CO 

tuoooooot 

LO        CM        O  00  CN  lO 

CO           T           1-HT 

C  lo 

t        LO        CO        CNCO        TO        »C  CN        0>        LOO        CN  t--        i-t 
CN        T        CN              CN        CNCN        CN  CN        T              CN        COT        T 

CN  oo  co  o  oo  lo        O  LO        OO        Oi  T  LO  l^  CO 
T  O  CN  CN  CO  LO         CO  CN         >0         HOHUJO 
0000O50000O5         00O5         00         0005000005 

OO 
00  00 

O         CN         O         LOCO         COCN         OCN         TJi         OCT         COLO         lO 
CO        CO        t^         TO        COT        I^T        O        t^O        COCN        t>- 
00         00         00         00  03         00  05         00O5         05         00  05         00  05         00 

c 

i 

p 

£ 

c 

1 

co 

p 

c 

E 

1 

c 

c 

V 

2 

c 

p 

p 

c 

\ 
X 

c 

-r 

E 

c 

1 

c 

p 

c 

■1 

c 

w 

p 

c 
g 

1 

P3 

p 

c 

1 

c 

P 

p 

c 

r 

p 

1 

P4 

p 

c 

= 

1 

pel 

pi 

p 
c 

p 

1 

Pd 

ro 

c 

I 

— 

c 

p 

o 

I 

1 

p 

p 

c 

g 

c 

i 
! 
i 

c 

c 

c 

CO 

i 

1 

- 

i 

5 

c 

PS 

CO 

g 

p 

IE 

c 

M 

1 

o 
P3 

V. 

i 

D 

c 

c 

c 

c 

p 

c 
P3 

p 
c 

E 

c 

TC0 

PS  P 
c  c 

ii 

o  c 

d 

lie 
m  P3 


^     ^ 


^       ^       £ 


O  CD 


o§   o^ 


c3  cs 

O   CD 

"S8 


as4  a& 

T  lO 


ft  :  ft 


o^  oS  o$ 

c3  PI   C3  PI  C3  Pi 
CJ  CD   CJ  CD   O  CD 

llllll a 

<1       <5       <J       «*S 


C3  PS 

O   CD 

Ti  a 


PtS  PltS 
03  CS  o3  PS 
O   CD       O© 

■eg  "c a 

Bo  So 
<3     <J 


Q   :Q   :ft 


P3+2  pS+f  Pl-g  PS +3 
c3CSo3Plo3P  03C 
OCDOCDOCD       O   « 

ill  is  i  ii 

««J    <1    <     < 


■   Pi 

•     03 


o£  o£  o£ 

pj-g     PS+f     ps-g 

03  PS      03  PI      03   P 
O    CD       CD    CD       O    CD 

•c  a  -c  a  "c  a 

2ft  2ft  2ft 

So1  a o4  a o 

<      <     < 


5S    \ 

ft  : 
»d  : 


Oq  Oq 

03  PS  03  O 

O   CD  O  O 

b  a  -c  a 


t^  GO 


PI 


a 


—18  G 


274 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•&[8jxeq— lonpojd  rerjrai 


•183j— q^dap  \mo& 


•^aj—qidap  no 


o 

I 


'188j— dwa\d 


•%Q9} — \ZAQ\ 

■Gas    Avopq    apr^i^V 


•189J— 

pajBjjanad  ssaujfoiqj, 


•;98j— do;  01  mdaa 


sz 


1    - 
N   ft 


a>  oo  oo  im  oo      a>  as      o>  t- 


CO  Tfi  <n  co  • 


^lOOOO       oo 

~  t>  co  gj      co  io 


oo  c-  oo  oo      oooo      oooo      oo 


o 

03,Q 


5-° 


OS  00  .-H  «D  OS 


rHNOl'O'l 

CO  CO"*  CO1 


CSOS      -(MO 


£8S?32 

00  00  OS  00  OS 


i-H      ,  CO  i-l  CO 

g  ;'§§§ 

ot3  o  o  o 
P5    ".P5P5Ph 


r 


g?co 
00  OS 


O5C0-H 


8££ 

00  00  OS 


<NCO 

a  a 

,  o  o 


tftftf 


S8      §8 


t-     00         00 


t~<M.-H«0' 


TH     CO 


N 


<M 


£  £     £ 


£       £ 


HO  CO 

dodoood©    °. 
o       d     flrtnf  Art  flag   g     S    S 
-   !2  S  2  i2  S  i2  S  m  "So 

*  ^        c3  c8  03  53  S  03  (3  O     O 

£     ^   pQQoopoa w 


M    M       bo 

P     P      3 
o    o      o 

www 


b3  a 

•s  a 

g  o 


s-p 

03  1=1 
o  a> 

'5  s 


o  o    o  o    o 


Oo  Oo 

tf-s  0-p. 

03- fl  03  P 

o  ©  o  <u 

"Cg  'Cg 

g  o  g  o    S.'gSSS.'SS.'S 

<<  <3  £&  pen  fe  fx,  'pq  pq  pq  Jj 


>^^I>>I>>!>1>>>)^       >>>  >5 


o  o 


A2 

3_ 

i— l  <M  CO  "tfi  io  <»  t>  00     OS 


o    . 
•rt  O 


BLATCHLET] 


TABLES    OF    WELL    DATA. 


275 


as 

05  o 

05  t3   05 

issi 


oc£ 


£-  «tt  a  S  a>oo  J3 

-<N     ^O     _0     „^ 

co  O  co  O  co  O  co  ■*■? 
03  0  C3O0  05  Ol  o3"m 

O     O     O     Oib 


'  *T 

- 

:  «s 

03 

£ 

■* 

* 

c3 

*■  03 

03      . 

DQ 

.02 

02      . 

•          +B+S 

'■^ 

49       • 

:    l 

% 

:S 

a  : 

505        OO  SJOoJlCl  o 

-05     Noeo«Ne 
d*"      o> o **-  05 ^"  oo *" 


tO    K  UJ    K  TT     KIN 

03  03O  03  Oi  03O 

OO    o  •  o 


03  OJ 

O 


OOOiO 


22cn 


■PS 


bS       8! 
ft 


CO  00         00 


oo 

SoS 


lOiONO' 


8  :g 


NMMHH^OirtONt-CCCCCOOlMMC^OO 
MOCOTl<0)1000tOOOiOO)iOTI'0'*OOOHO! 
HHi- 1  ,— (Oi-lOOi-HrHOO'-Hl— 1  1— 1  H  i- ll— lO 

r^t^OOiOCNcOO 

(M^H00i-H-HO0Tt<r-l 

-r  —   ~    ~ 
CNCOCNCO 

HHHO> 

O  CO  00 
NOh 
MOH 

00  00 

88 

00 

o 

o 
o 

eor--t^CJ>c3JcOi-(a50eocOTj<cNt--!-ir^t— eotM 

NrftOiOO^HMINIiOViOOliOOlHOOO 

cocoeoco"'»<co"ct<'<j<coco-cf<*'cocococococo-fl< 

nwooiooo^o 

NOONOJOOHlOO) 

coco^coco-cpcoco 

CO 
CO 

CO 

CO 

(OOHrt 

t^  r~  r^  co 

CO  COCO  O 

1-1   TftM 

t^  05  00 
t-OCO 

CO  o 

00 

o 
■«S1 

•*(0t>.iCKIQ0Q0tN00CS"OiONiOCDHlClO 
IfllNH^HHHlNHHNHCqHlO 

oooo 

co»o        

1C 

oomio 

CO  CN  "*  *si 

§  ':  : 

lOCM 

TfC 

o 

^ooooooioooooNcqMinoHNOtoft 

ONWOlH»OC»INX(Nc>5  00NtOOtO(» 
OCOOOOOOOOOOOOOr^OOOOCiOOOOOOOOOOOOOO 

00OOX0OW00CM 

lONOr-NOcoi^ 

0000050000050000 

'.2 
oo 

00 

862 

856 

855 

1,045 

lO  00  lO 

t~  (N 

^H  02 

o>  oo 

1 

00 

2-cj  o' 

02  :« 


I  .-i  CN  CO 

>  o  o  o 

J    C/3    CO    CO 

!  9  9  9 
!  3  2  3 

)  o  o  o 


rH  cm 

i  h 

z  c 

3  8 
fl'l 


COrHCM, 

el  rt  d 
o  o  o 

»!  »  to 


a  q 


CN-H 

as 

O  O 

CO    CO 

fl  PI 


c   :  a 

o    .  o 

CO      .    CO 


>»  ".3  .3  ".3.3  '.3  P--.S 
,0.0.0,0,0  030,0  0°£^°J2  C3.0 
OOOO  O  Js'd  O         0"d   O  O^  O  J3  O 


O  o  o 
'd'd'd 


«tf 


CO   o 
00    t- 


)  00  OO  00   OO   OC  00 


COi-H   <N 


£   55 


W  W   W 


oooo    o    o  o 

o 

o 

o  o 

c 

o 

6  6 

i- 

zzzz  z  zz 

55 

55 

5555 

55 

55 

ZZ 

55 

XX.CC    ^5    XX 

^ 

■d 

.dX 

A 

^ 

'S'S 

Tl 

fc 

oooo    c    o  o 

a 

o 

S& 

* 

k 

o  o 

O 

T- 

£  £  &  £    £    £  £ 

* 

£ 

££ 

£ 

* 

t£|£ 

^ 

C 

■d 

■a 

-d-d 

■d 

•a 

WW 

5=' 

> 

oooo    o    o  o 

- 

o 

o  o 

o 

o 

^^^^  £  £<: 

£ 

* 

££ 

^ 

^ 

i-»i-» 

H,' 

« 

6 

d  ■ 

d 

d 

o 

d 

d 

O 

U 

O 

O 

O 

CJ 

O 

c^ 

3 

c3 

g 

3 

CO 

C3 

3 

O 

o 

o 

o 

c 

u 

c 

=3 

=a 

-a 

^ 

4 

■a 

=<j 

O 

o 

o 

o 

o 

o 

o 

l>. 

>> 

>j 

>> 

>» 

>> 

05 

05 

05 

05 

o  o  o  c 

c     o 

C 

C 

c  c 

c 

C 

o  c 

c 

C 

X! 

XJ 

^2 

& 

,Q 

^2 

X2 

xl^^x 

A   ,d,C 

X 

X 

x:x 

X, 

X 

AX 

- 

XI 

hI 

t-1 

J 

1-3 

J 

h-1 

hJ 

OOOC 

O   OC 

C 

c 

OC 

C 

C 

OO 

O 

O 

CO 

IQ 

CO 

t^ 

00 

o 

t- 1  CNCO^ 

■o    cor- 

cc 

Ot 

o»- 

CM 

CO 

iH  CN 

re 

l« 


276 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


■sjaireq — ^onpcud  papui 


•laaj—ircctep  lino  j, 


•}99i— mdap  \)0 


d 
<s 
•d 

« 
pj 

o 
O 

I 
■§• 

pSS 

oo 

© 

© 

J, 

■ha 

O 

O 

I 

Q 
'~ 


inn^'Bp  aAoq'B  apn^my 


•188;— I8A8] 

A\opq    apn;i^y 


•}99j— 
pajBijaued  ssaujpiqj, 


•;88j— do^  <n  t^daa 


l*s 


.§538.1 


c3  03  o3  O  c3  03  < 


LOOM        «5iO 


OiOOOiO<CMOOOOiO 
r~t^cOCO-3<C2.-i<Mi^i-ICO 
05000500500050000505 


is 

£05 

MO 


lO  00  CO        05  < 


HNM        <M, 


OOOM       O  lO       in 


r-  i— i  co      coo      o 

INCOf         CJi  (M         CO 
05  05  05       05  05       05 


«  :«    tf 


oo  o  »-i  co  t~  oo  oo      <Nio^Tfi-H^H 

1-HOO-HO.-IO  i-IOtHOi-HO 


:^S2 


10(N«000  00 
c/  re  I  ~  CO  t^  CO 
00  OS  COO0  00  ©5 


cV,S  O  o3'3 


03.Q 


H  o 

«3p4 


o3,Q 


CN05  05 
iHOO 

lO  lO  lO 


NHrotovotoooNH    oo    re    co 

O  O  05  i-H  i-H  05  O  00  05  O  1-H       00       O       i-H 

io  m  T  w  m  -^  io  ■«*<  rji  in  io    rf    m    io 


6  6  6      6  6 


co  -"tfn>  oo  cm 
6  6  6  6  6  6 


.-H      CO 

6^6 


AAA 

Wicyotuo 

2  2  2 


,d.d 

bjcfcx) 

aa 

03    03 


7ggug  uu     .     ,     ,     , 

Moooooodddd    d    m    d       n 


CJ.1^^   ,3,   ,£1,  ^  ,£*  ^         .>       .,       ^       „ 

jadddndd^caosos    a 

*■  *|MMMM     *"' 


i    fc    £ 


p.      w 


fcP=Hpt|         fef* 


H         1-3 

.S^^^^^^cjooo    *    C    o      o 


e  a 

03        c3 

pq    pq 


o 

03 

1 

Ph    • 
C3  O 


■j3  o 

02 


.2.2.2.2.2.2.2.2.2.2.2  -2   ®   ® 


2  2  2 

233  ^^  ^^.d^^l^lrf^^^^  C3  'O  O  "O 

OOP  OO  OOOOOOOOOOO  PQ  FQ  PQ  PQ         CQ     O 

i-(  CN  CO  -^"5  CO  i-H  C<»  CO  Tf  IC  CD  t^  00  02  O  i-H  CM  CO  ■*      lO    CO 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


277 


8-3 


l-H  Ol-HO 


aooooo 


C3.Q  C3,Q 

coPhcoPh 


o    o 

C3      03 

S   E 


«    B      ffl 


P>H 

h 

Ph 

=3 

=3 

4 

>> 

>> 

>> 

sa 

-i 

03 

pq 

- 

« 

X 

— 

3 

■sjajxeq — ^onpoad  ibijtoi 


•}99j— T^dap  ibjox 


•}99j— qidgp  no 


199J— QWS\d 

mn^Bp  9Aoq«  gptm^y 


•199J— I9A8J 

■B9S    Aiopq    gpn^jy 


•}99J— 
p9}EJ}9U9d  SS9U5[0TqX 


•}99j— do;  o;  qjd9(i 


co«2«  >.2« 


££ 


c  . 
33  c 
2fc 


CcO 


b8" 

A 


2  "3 

Oco 


§ 
®  3 

3.0  O 

•3£°* 


b2 

Q.SP 

h3 


■  NOONtOONOlrtOHlONO'fl'Oim 
iHffiWNH-NXNrCCOOSN'H 
>1-HOi-t>-t»-i©i-i©©OC,q.-iOOO><-i 


O  *-«  cc  y:  -l  ::  —  C  s  s_  — ■  —  ~  '-t  x  3  cc  —  r- 

oot^oxci-i-r./t n  c  c  r.  o  c  m  x 

COCO''3<CClOCOCOCO''3<CO"tf'' 


I  CO  lO  T  m  cc 


lONONOiaHHI 

iC0OOO«XC:CC-.-.^.O^QO0!O( 


h  c 
mP3 


CO      .—I  .CO 

i  :«  :g  . 

O     .  °  .  °  !> 

CO       "    CO  71   ?    ff)   71 

.5  >>S  '.5.2.3.3 


r-HCC— HCO 

o  o  o  o 

CO 

a 


O  C3,Q  SOO^   C3X2°^1§^^^^  C3 

T)^oi'0,Oo£o'Oo"ooooi 


CO  ! 


CC  t-  Tf 


>o    t- 


IN    ©     f 


X 


O      ■   O  O  O  O  O  O00 

c/T    -.  c/T  co"  co'wT  co"  co£^  ^ 

S  O  O  ©  ©  »  ©  *  w~  <yr 

^^i^i  in  Si3  ^  £i  ©  © 

C3c3c3  C3  O3o3  03  C3fl  H 


c 

rfi  ^    odd 

o  a*  ^  ^  ^ 

©  O     o  o  o 

g  3  '3'3-3 

g  Pn   O-O'O' 


222    2    22    2    22    2 
232  2  22  2  22  2 

ooo  o  oo  o  oo  o 


i-i  CN  CO     tji     iO  CO    t^ 


CO      to 


278 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spjueq— jonpojd  veiirai 


©  aX3 
Sis  o 


coceZ 


of +5 

Oco 


•^eej— mdep  i^oj, 


•}88j— q^dap  no 


■%99}  —  autqd 
xniUBp  8Aoq^  apnqjp/ 


'Onu:cN 


o>-ia500ooo< 


■B9S   Avopq    aprimtv 


r^      oo  io  "jC  z: 


OMCOMOOOC 


OHO00ON0)0>HNi 

c©oo-^tc>ootocc>r~coiOTjisocOTT<t--coaocoi 


pe^Bj^nad  ssaujfoiqj; 


!0«nco 


ONOJN 


lONlOW 


•^09j— do;  <n  qidea 


^    CO    CO 

o  q  q 
Is  2  2 
coPntf 


oooooooo 

,^32.5  55959 
2  5s  S  3  3  2  2  3 ',3  2 

OJ-OOOOOOOO 

tf  co  Ph  P?  #  tf  g  P5  tf  PS 


q  q  q  q  q 

o  o  o  o  o 

to  CO  CO  co  co 

q  fl  el  fl  q 


:  q 


'  o  o  o  o  o 

:p2tfp5p2« 


»3  c 
doPh 


:  q 

,  o 

►J 

C30 

is  o 
coPh 


3  2®  f3  S® 

rT^.C3     ffi     >     O     © 


77 

33  o 

CO 


lO  CO      OS         lO  -*f  CO 

CM  CN     i-H         <N  CN  <M 


8      2    8 


c 

c 

rt 

<M 

CO 

c 

fc 

TP  CO 

ft 

43 
ft 

o  o 

T) 

;>>:>> 

- 

a 

q  q 

pj 

s 

©  © 

s 

« 

MM 

cs 

£     55 


£    £     £    £ 


W    W 


ltd 


©  ©  03      ©  _ 

,q       ,q,q   ,q     .2 
to       .J2.J2  .^3     ,q 


.23     .2 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


279 


83 


o  >  c 

GO 


O  03 

5ZO 


c  "O 
55 


°  °.  «8"e8 

55  55Oc0 


<°  .J    ■ 

Oi'O  +j 

-2  © 
Sg-2- 

Oi    £    §05  0 


©  S-  c  ©_©. 


+3  +3  K  O  OT~+3 

co     co     55        •     Oco     OC 


-S'CSi'd 

S3  o*  o 

-£    -2 

055055 


P.P, 


E,'     ,d,r5  C     £h'      &"     £?      <§.d      <§« 

p         fcJO  MQ        p        p       p       O   M      O 


^P    ft 


CT-O 


00  CO        co  cn  ro 


lO         NrtO         O 
iO       i-ir-io       o 


CO  CO         ^H  t^  CD 

28    2cS 


C5  t-      o  coo 
^O      -<o© 


TfiOOt^COOS^HOlCN 
IO  M  ffi  lO  IO  ^  N  ■* 
CO  ^3*  CO  ^  CO  ^  CO  ^ 


CO  iO  -^  -v  IC  CO 


OO        OOO 
CO  TJt         CO  •"*!  -W 


•  CO  i-l  CO  CO  CO 


SO  *■-  CO  CC  ~  I    s 


05  030 


00©  tN05< 


9  :g 


is  ° 

coPi 


03X3 

+3  ° 

coPi 


£  c  £  o 
ccpicoPi 


>-..s 

C3.0 

h  o 

CO  Pi 


.2    >:.H 

£2  C3X5 

Pi  CO  Pi 


coPi 


11 


03  Oo 
J--0  O 


£5  O 

o-b 

tf  : 


co  Pi 


ggg 

io  3  3 

ooei 


io  "0  io    io    »o  m    io 


pq 

«    Pi 


55    55    55 


OOO 

55   £   £ 


5    s 


i  o  o    o 
i55£   55 

fgcT  « 

!  03  03      c3 

as  a 


OOO 


—A 

o  6     „ 
5555    $ 

as  ° 

©  © 

OP 


o  o  ., 
£55  © 
cfd"  o 

o3  o3»-» 
©  ©     . 

OOO 


o  o 
5Z£ 


OOO     .     .     .  ^. 

vi  w  xr.     '     '     „  ^J 

©    ©    ©  4^  +j    ©  © 

c  c  c  f-  s-  >  «n 

O  O  O  e3cJi.  © 

.    C    C 


O     O    o    PO     ^^^pipi§  ^ 


III 

«     H     PQ 

'O'       "^       "O1 

©      ©      © 

Pi    Pi     Pi 


o 

3  3  3     3 
ooo      o 


►JJ_3   J   OP   ^ 


C3  C3^| 

PPO 


03  03 
CO 


oo 

— i^h         •    •    •  o  b  m 

*j-+3  ooo©©  "3    o 

©©  sir 3s£  « 

OO  OOOcocOh,   O 


o         ^H 


N 


IN        CO. 


INM*' 


<N 


^    ^     ►    ^    £    H 

55     co  I  co  I  co  I  co  I  55 


I     55 


280 


OIL  FIELDS  OF  CRAWFORD  AND  LA  WHENCE  COUNTIES,    [bull.  no.  22 


o> 

..s 

(=1 

O 

■o 

I 

CO 

1 

I 

o 

CO 

« 

rO 
O 

© 

i 
i 


o 

•  i 

JC 

•  o 

Tf 

:  g 

:S 

3 

.  c3 

■  c 

:S 

CO 

a 

!*« 

:» 

•O 

S 

;   •  a 

a 

.      -d 

.       S3 

o 

•    -d 

5 

e 

3 

i^ 

1 

1 

■    CO 

.  *-• 

o 

Ii 

.  CD 

:  ^ 

:^co 

IS 

03   -s 

03  « 

oco 

■qi  o 

^  o3   ;  c3 
t-o    ;o 

.  c3 

:° 

,rc3  K 

s 

CO       f> 

O  03  03^ 

I: 

O   c; 

09 

«5  :6 

o  o  :  o 

:d 

:1 

•dft    : 

:§l  : 
•co      : 

:coc 

c 

KO 

X 

- 

tt 

:!zi 

:}z; 

•  f^Cf 

>5          «= 

>> 

J 

>> 

l-c        r- 

t- 

•spjjeq— lonpoid  im^ui 

•  A 

ft 

ft 

00 

ft 

ft 

t-        C" 

oc 

•  ' 

•     'O     -o 

TT 

CO          CO 

» 

« 

•       •  -*ti       -CO 

•iwi— q^dap  unoj, 

o      cr 

CN 

"1.   '""I. 

o 

T"H 

^ 

•  •  00 

•  -co 

CN 

CO 

■* 

| 

O      'O 
CN       •  OC 

•OCO 
•  in  en. 

o 

•iaaj— q^dep  no 

.      .05 

o 

a> 

O     ;05 

;C5  O 

OS 

;     ,~' 

•;aaj— auB^d 

CN  CO  C7 
OOC 

co  en  a 

£35  00  l^ 

CO  CO        CC 

CN  C5          OC 

I  - 

CO  OC 

■OCT 

s 

2 

O  iO  O  CO  •*  00  ■*        to 

rHCOiOCNCOCO^            T* 

ONO         . 

Oi       c 

OCT 

O 

— 

- 

O  CJ5  O  Ci  rH  CJ5  1— 1          o 

rairvep  sAoqe  apnmiv 

HOC 

I^Hp- 

f-  Tf             l> 

:■- 

■*  CN 

l- 

CN 

CN 

1 

inONfflNffl         Tfc 

•^8J— 19A8I 

NtDr- 

Oi-h  CN 

c^o       .- 

5C 

"»<C 

c 

CT 

(OiONMtOiO        m 

tj<  rt<  Tt 

•*i  C^  rr 

CO  lO          T 

CO 

■*  IC 

l> 

iC 

IC 

o  ■<*•  ic  co  »n  co      ■»* 

B8S    Aiopq    aprnrqy 

'-  If 

CM 

CN  ir: 

S 

u; 

t-NOCOO*t>        00 

•»99j— 

i-l  tM 

•     • 

1— 1 1" 

^ 

CN 

ti>  CN  CO  CN  CO  i-l        rH 

pajejiauad  ssgnjprqj, 

mmC 

C5  CO  oc 
-i  :-   :■- 

c 

r~      t- 

§ 

NC 

■  r 

<= 

c 

CN 

lOOI^OtDW         CO 

OS  Of  C- 

CO         CN 

t^  c- 

S 

e 

05  00  O  I—  O  00        00 

laaj— do;  o;  q^daa 

05  0  0" 

OiC^a- 

5 

o     a- 

CX 

OJC 

5 

OO01H00O00       Oi 

CO 

'H 

1-1 

1       cv. 

£ 

C3 

CO      ll- 

'.    !cn 

CO         i— 

CNCO 

c^ 

c- 

Tf'  <N  t}<      ;  rji 

CN 

fl  :  p 

:  :  p 

d     p 

fl  p 

C 

E 

fl  p)  pi  p)  : 

d 

Pi 

o      c 

.    •  c 

o       c 

o  c 

c 

c 

c 

o  o  o    . 

o 

o 

% 

J. I 

:  :l 

> 

co        V 

B     £ 

> 

,    §£ 

0 

V 

!P    t«    OJ    1/3       .CO       .            CO 

S  3  S  5  >>9  ^   .9 

•p^-p 

•§  ii 

ef 

"&     ft 

c 

22 

IS 

X 

3SS3  os 5  c3    2 

ofl  C 

o      c 

t- 

o  c 

c 

c 

oooo>-.o«~,      o 

ft  :ft 

:  :ft 

£ 

ft      ft 

cc 

PhP^ 

Pi 

Pi 

C4  Ph  pi  p^  CO  ft  CO       ft 

a  o  o  o3  d  <£ 
02,2  C3  >.2«£ 

^^ 

. 

sr—^—,^^—,r— . ' 

**oc 

CN     I> 

■o        o      < 

» 

c5~ 

Q> 

r>     o      Tf        cNt 

CNCNCN 

CN     — 

■O           t- 

N 

CO 

■o        CO        CO           CO 
O       lO       iC          >c 

mmiC 

lO      IT 

C           "" 

tf 

C 

iO 

lO 

9 

* 

CO 

o 

CO 

--1 

^'      TJ.'      ft        ft 

"3 

6 

J        c 
o 

6 

6 

6 

o      6      6        d 

03 

1 

^^ 

«H 

5 

& 

z;    ^    »      Z 

.J-OC 

1** 

6   *" 

5    g 

b     p 

c 

d 

"3 

t-T     tT     tT       ^r 

CD         CD         CO            CD 

pi     fl     a       a 

cd  s-T  ;- 

H 

r         a 

Ej 

i-l             (-            i-                 (H 

®oc 

■2   p 

§3      -c 

p 

% 

5 

c 

3       D       EJ         Pi 

^   CO    K 

£  1 

§       I 

«          DC 

f 

[ 

pq 

s 

q     ft     PQ       cq 

£<        Ph        pH           pL( 

>> 

§ 

d 

£■ 

S      d 

fi: 

^ 

o 
o 

0 

o 

o      o      o        o 

o 

o 

O       O       o         o 

EEl 

o 

{ 

q 

ft 

=P     ft     ft       cq 

"8 

a 

o 

1          1 
C3             Cv 

-1 

5 

- 

a 

•8 

Pi  ' 

8     -^     °8       «8 

co        co        co          co 

1 

.22 

3q       pc 

PC 

5 

E) 

cc 

3 

5 

CD        "CD        'S           *© 

3      D      d        d 

03 

ooc 

332= 

S   C 

<c         a 

a 

s 

c3. 

1 

i 

a   a   e    s 

c3        c3        c3           c3 

ooc 

tf        P= 

p: 

1 

/. 

OD 

i=> 

O        CO        CO          CO 

p*  • 

c?0 

CM  CO  -^ 

r-H      O 

CN 

eo 

^        iO        CO          t^ 

S£ 

§  . 

T3  o 

* 

£ 

[ 

*i     ^ 

^ 

* 

4* 

DQ 

i 

Z5   ^ 

oi- 

1      «: 

•H 

»H 

CO 

BLATCHLEY] 


TABLES    OF    WELL   DATA. 


281 


o 

rd 

1 

■*■> 
3 

OS    V 

si 

o 

1 

c 
c 
C 

c 
a 

i 
e 

' 

o 
o 

<D 

1-1 
o 

C3  O 

is 

--  £ 

-  c 

— '  e. 

a 

c 

a 
<I 

c 

CO 

- 

a 

,c 

IK 

r 

i. 

O^rrj 

Lp 

co  C 
C3TJ 
"P 
rr-J    0 

o-9 

O  C3 

a 

E 

> 

1 

'cc 
EG 

■  c 
1  c 

:^ 

—  -r 
00  00 

15 

•  © 

as  t^  a: 

•"OS*" 

,<M     ~CD 

CD 

s 

CX) 

co" 

c3 

C3 

A 

ft   ft 

>> 

ft 

ft 

IO  IO        IO        IO 

io  co      ii      t>- 

g 

CO 

I 

8 

cr 
o 

CM  CO 

00  CO 

oca 

oo 

o 

CO  as 
Osoo 

>0  Tt< 
CS  00 

00  OS 

JO 

CM 

35 

o 
o 

o      o 

ii         CD 
rH          CO 

CO  tr^ 

t^rH 

OS  OS 

o 

os 

l> 

8 

o 

X 

OS 

■<*<  io       o 

OS  Tf            CO 
CXJCO         OS 

CO 

1,115 

1,054 
1,112 
1,079 
1,046 
1,131 
1,116 
1,152 

965 
1,145 
1,062 

972 
1,115 
1,155 

989 

CO  OS  lO  CD  t-  00  CN 

CO  >o  CO  CO  IO  CO  00 

lO  -f 

CO00         CO               OS  t"^  IO  "C"         CO         IO  »0  Tfi  IO  tti  1< 
00  CN         CO               f~  CM  OS  TP         T»i         HlOHCOHm 
OSOS           O                  OHOH           O          H  O  i-H  O  1-H  11 

00         -f  00  CM  tO  CO  00  T}i  CO  IO  CO  CM  00  Tfi  rH 
CO        ■<HCOT>''Cf<COCOCOiOCO''JiiOCOCOiO 

-rjl  rH  lO  Tfi  CO  CM  00 

CO  TP  CO  CO  ^f  CD  1 

CO  CO  CO  CO  CO  TT  io 

TJ1    Tf 

C^CN        CM              ilCOLOCO        !>•        lO  iO  CO  lo  (O  CO 
HN        CO              NWOiO        lO        OOThOC.  CO00CO 
LQ  lO         Tfl               IC  CO  Tf1  CO         ^         CO  "CP  CO  rr  CO  CO 

JO  OS  O  OS 

cm 

IC 

OS  IO 

OS  CO 
TtKM 

r~  io  io 
IO        n 

O      -OOCM 
CO      ■  Tf  CO  !>■ 

t»-         OONOCOCiOONiO»00'*'*0 
rH         t^HiOOOO)ONiOOO®OHNt< 

O      os  os  as  as  oo  os  co  o  coos  o  os  oo  o 

O  N  *  O  O  Oi  iO 
OS  *0  t--  00  CD  (-»  CO 

00  00  00  00  00  OS  o 

co  r~ 
lOCN 

OSO 

OiO        O              lOOCNO        O        NONrtNN 

io  o      ii           ii  co  os  rfi      t^      t^  »o  t^  io  i^  r- 
On       O            OCOCOCO      OS       ccosooosocco 

> 

(■ 
ex 

CI 

i 

'j- 

2 

0 

- 

> 

X 

P 

c 

■j- 

.3 

— 

0 

P3 

Pi 

c 

BE 

c 

> 

c: 
- 

0E 

c 

-f 

p 

c 

p 

1 

> 

c- 

-7 

e 

c 

co 

.  P 

c 

£ 

o 

03 

F 

'1 

> 

c- 

(- 

1 

CO 

1 

P3 

> 

a 
•7. 

'c 

c 

* 

c 

c 

t 

«: 

c 

CO 

p 

ic 

c 

p 

c 

F 

1 

R 

p 
1 

c 

- 

i 
c 

CO 

c 

Pi 

= 
c 

p 
IE 

o 
Ph 

-r 

p 

c 

p 

rC 

c 

pi 

i 

0! 

p 

c 

p 

c 

C£ 

2 

c 

P3 

~  c 

> 

s 

i 

V 

c 

Pi 

;    ■    ;    .e~    ; 

;  cm  ;  co  n  : 

,  o    ,  o  o    , 

OS       OS       CM  CD  CD       rH       rH 


OS       00      CO 


Z      !25 


CO      rH      rH  t~  CO      rH      CM 

6066666 

q   pT  pra'a"  fT  pT 


Z    g  ^  £££  52;  ^ 


n     n     <N 

6    6    6 
K  X  Z 


o    o 


see 

H      H      Pi         «>      4> 

Si        Si       Si  >        > 

3     3     3       OO 

pq   pp  pq     o  O 


fe   <  < 


§  S 


0 

c 

O 

O 

Orjl 

fc 

? 

Z 

r2 

^6 

rd^ 

-p 

rd 

^ 

rd 

bfi 

CJ) 

CJ3    ^ 

3 

3 

3 

r 

3  co 

rQ-2 

a 

ad 

1X1 

OS 

rO 

■fi 

rQ 

rQ 

v-'ts- 

fc      r?, 


S   S     S     StJt   pt   ^^ 


3     3     3  3 

>  >  >>: 


s  rt 


9  <o  CO 

rM  &JD  SjO 

3  O  O 

P  Pi  Ph 


3 

.g.s  I 

§  §   ■a 


r3       r3       r3 
OOO 


OOOOO 
2r3      'r3      'r3'r3 

OO   O    OO 


282 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sjaxreq— lonpojd  repini 


•}88j— tucfepiejox 


ooo"—  ' 


CO     £ 


■588j— mdop  no 


a. 

•d 

d 

d 

o 
O 

I 


•;98j — aire^d 
umiBp  OAoqe  9pnmiV 


■  oooooooo 


•}89J—  \QAQ\ 

Bas   Ai.opq    9pnn;iv 


•189J— 

pa^nauad  ssau^oiqj, 


q88j— do;  o;  mdaa 


00O        OOCOOiOOffiONffiX 
00  t^         lOiOtONMNTCCtO 

00  Oi       00  05  o>  o  o>  o>  o>  O  Ol  00 


xS     >v2. 


COCN 

a  d 
o  o 


cS.a 


d  a  a  d  d  d 
o  o  o  o  o  o 
co  co  co  co  co  co 

SBBBB.9 


o?2  IS  o  3  2  2  2  2  3 

_£-  O      £  O  CO  o  o  o  o  o  o 


NOlOlOMCSMM®l» 
Oi— li— It— I  O  i— I  t-<  O  i— lO 


OOOliMONHOlNtfM 


iOiO«iCOCt^NM» 


O300O50CO50000O> 


II 


d   :  d 
o    .  o 


9  :ff 

o    .  o 


.2   >-..£    >*£    .    . 
,Q  03,0  03,0  <$0£2  jrj^j 
o£0£0_>3t3o.J-0 


©III. 


to    CO    «o 


(CrfOOCONNO  CN  lO  <N  CC  CO 
00O00O=(NN(N  CN  ONNO 
•«}<  lO  •"*<  tj<  10  lO  »0     lO     lOiOiOiO 


CI 


H     t>     M 


o    o    o 
£  B  £ 


o    o 


o  o  o  o 

'Z'Z'Z'Z  ooooooooo  o 

co  co     to      CO        co        co     co       .isj^^J^  _    „       „       ........ 

O             ©22        2        22        oooocococococococococo  OT 

g       ggg    g    gg    £§§§©'£©'  |  ©©©©  S  jj* 

£       £  £  £    £    £  £    £££*:£*:£  £  ££££  £  £ 


•13  o 
©^ 

02 


o  o  o  o 

3  3  13  3 

O  O  O  O 

h  w  n  tj< 


o    o 

3  3 

o  o 


ooooooo    o    o  o  o  o  _o 

3333333  3  3333  3 
ooooooo  o  oooo  o 

t>00O>CHHN      CO     "*<  lO  CO  !>•  "00 


BLATCHLEY  ] 


TABLES    OF   WELL   DATA. 


283 


iNOOlOffitMHTtilOtDNOLOOHNtDOOtOlON 
-h  (Q  rc  1*1  — >~  "*  !C  iO  CO  ■*  CO  tO  CO  -H  lO  CO  tO  CO  CO  o> 
!Ot-l05rHOT-(r-<OCiOOr-iC5^HT-I^H^HOi-H-Hr-IO 


«3C<5Mil5HtOOCO)CDlO,J,MHlOOO)»1,ClTPiOfO 
CO-^COlOCOTJiCOCO^lOCDCOlOCOCOCOCO-^COCOCO-*1 


>CO!      ■  O  S)  W  «■  iO  f  O      ■05  0500      •  <M      •  iO 


io»«ioo' 


_    _>  05  00  00  tO  CD  i- (OTFOGOOi— I  C> 

i  OO  X  1^  CO  N  Of.  CO  tO  00  N  rX  -r  GO  O  N  O  M  N  iO  X 
iOOO«ffl0000050H000000005000)QOOOOOOO 


o  o 


dqPh 


H  o 


h  P 
o  o 

00    00 

s  s 

S3 

o  o 


t*'-0  ^  .2.2.2 -°  <s3 

coPhco     !     '     '.P^cO     ' 


O  o 


3  8 


6 

*H 

CO 

Tl 

OJ 

<N 

00 

lO 

^ 

to 

O 

c 

o 

o 

O 

o 

o 

o 

o 

1? 

B 

5 

£ 

fc 

£ 

fe 

55 

fc 

4) 

en 

./: 

00 

00 

oo 

00 

00 

,0 

£2 

p 

,Q 

,Q 

,Q 

£2 

.fi 

,Q 

"3 

,fl 

xs 

p 

fit 

.Q 

X2 

P 

,fi 

£2 

t 

> 

Ch 

u 

u 

u 

o 

o 

O 

U 

u 

O 

©      05 

ft     Ph 
©       © 


o 

- 

A   J 

lJ 

J 

h3 

ri 

J 

^ 

o 

£ 

CM      CO 

s 

13 

to 

£ 

X 

o> 

Remarks. 

Salt  water,  870  feet 

Salt  water,  1,360  feet 

Saltwater,  1,668  feet 

•sjaxreq— ;onpoad  ibt^ui 

-r 

•}88j— q;dap  reioj, 

to 

6 

188j— q^dap  no 

to 

■00      . 

•  to    • 

d 

C3 

CO 

•}88J— OTBjd 

uin^Bp  aAoq^  apn^rv 

■w  Tf  ■«<  O)  to  IM  N 

00  tO  tO  TH   IC  Tf  i-( 

CO  i-H  tO  1(5  CO  CO  00 

"1881 — J8A8J 

B8S   Aiopq   spn^pry 

1,116 

346 

836 

951 

1,144 

1,158 

1.188 

•}88I— 

ps^aiauad  ssan^uiqj, 

eo 

■  our 

188J— doi  o;  q^daa: 

'tOOWOONN 
■"JNtCNtOOOH 

to  oo  co  •*  to  to  r— 

© 

a 

T3 
o 

o 

1 

P.C 

pea 

"Gas" 

Kirkwood-1 

Kirkwood-2 

Kirkwood-3 

Sur- 
face 
ele- 
va- 
tion— 
feet. 

00 

1 

3 

I 

fc 

CM* 

6 

I 

C 

> 

i" 
1 
•> 

i 

p. 

i 

o 
3 

3 

I    ' 

fc 

a 

c 
u 
pq 

p 

•9 

c 
p 

i 

F 
o 

i 

J 

Ph    • 
C3  O 

.-i               tM 

Section 
No. 

I82 

284 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.   £bull.  no. 


o 
o 

I 


.2 

Eh 

03 

2 

If- 

1 

©  a/ 

03   03 

<2«2 

o  3 

:| 

«2«2 

s..Sft 

O  IO 

■  "• 

O  1  > 

!  i'- 

oo 

"J*  CO 

00  CO 

*tL'c 

■  c» 

J 

:^j 

a 

00O 

;  i-i 

i-Ti-H 

'.i-T 

5 

1 

■  03 
<  03 

P4 

s-Tt-i 
a?  a 

%3   • 

!  03 

c 

e 

CO 

•3 

"c3  c 

c3  e3^ 

^"3 

co 

OS  03 

; 

!  e9 

o 

•f 

£fc 

SftPQ 

££ 

:? 

is  13 

:^ 

r-T 

Ii-T 

+J  * 

■  +j 

:§" 

"OS'S 

'cl'3 

I  "3 

J 

3  c 

; 

:"c3 

C3       S 

tocc 

02 

COCO 

■  CO 

CQ  DC 

iQQ 

0 

O 

:o 

c 

•  io    >ou: 

•  >.CNC 

o 

•  »o 

•  i> 

;0<C 

•   Jh >-  CO         O 

•  Tfl 

•spjj'Bq— icmpojd  i^i^rai 

;pf 

c 

§£ 

:§8S 

•  Mine 

die 

•O  CO      • 

•  o  o  c\ 

00^ 

•lO  CO      ■  <N 

•;88j— x^dap  i'b^oj, 

i- 

5C  1- 

■CO  l> 

•  o  O  l> 

•  oTi-Tt- 

Tfl  Tt 

•  rf<  O      • 

9> 

i-HCN 

•OO      -IMOC 

t^ 

•  CO      <      • 

■*ti  CO       'ION      • -^l  O  <CT 

CO 

•  CN 

•;88j— q^dsp  no 

coo     •  OCC 

■  O  N!£ 

•  TJ1 

oc 

O 

OiONOCOiOOMNOONOOir 

cr.  <N^cc 

OKOOfflOlOT 

•;88j— aireia 

oc 

os 

o 

inaomH^NonocciooipM'ONNN      •<*<  co 

(M  CO  iO  t~  CO 
O  «">  O  i— 1  o 

rar^Bp  SAoq-e  epn^piy 

^v 

rf 

oc 

o 

OlOMOOlOlOONMCqoONlOH(y.»N        i-H  Tt 

O0  •<*!  1-H  r-t  CO 

•^98J— I8A8J 

-<c 

L0001NO)lON(MTt 

H*ffl'*lOO>ClNN         intONtD^NM 

eo  Tt 

lO 

OiOi- 

CllOX 

WHr 

roowcii'M^ 

■B9S    Avojsq    aptnmv 

oc 

lOlOC- 

o  c 

IO  iO  CO  o 
(NCNCN.- 

«NOOOO)Q9>e 
NiOOOMIN        CNCN 

OONNiniOiO 

•189J— 

CNC 

1— 1 

co  c- 

l><M 

i-l  i-l  CO  i-H  CM 

*d 

paiBxjauad  ssaujprqj, 

oc 

o 

OKJMOOlOiOONMI^ 

iO  O  O  iO  (N  O  O       NOOOiOOiO 

s 

C3 

rr<  c 

rri 

0O  COO 

3S  l- 

Nll"*tDMlOH«3!00'*ai« 

HM 

•^88} — do^  0}  mdaa; 

OOC 

O 

TttlONNr- 

cq  co  ■*  io  to  tc 

HtOtOMSfflffl       rr>  *J 

CO 

'H 

-d    '• 
Pi     ■ 

d 

1 

ft 

C3     • 

'^-Iim' 

'     !  (N  rH 1  CN 

8 

H 

1 

i 

i|9 

d 

c 

S"g 

l>&2 

g'gcJcSS 

ft 

03 
SO 

-d  c 

2  > 

c3  et 

c 

■1 

03 
6X, 

tl  c 

o 
•1  c 

fto 

03   [> 

■  ■^  o 

oo -^  c 

c 

■  fto  ft  ft  ft 

.   03    fe-    03   03   03 
O'O'^'d'dTJ 

■Cc 

■CPq 

0£-" 

"Cc 

£  3  S£ 

a-c 

■C.fe'C 

"dtS'C. 

pq 

pq 

soot* 

PP 

otPPPQk 

M 

P2  W 

:^w 

pqMpcpqpq 

< — ., — ' 

( 

N     ■*     CD 

••     03     l      r            .J 

o 

3 

u, 

■»f    "*"  cs 

i-<  CC 

eo 

CO  IT 

tO      KJ      11J 

iO 

to 

n2 

lO     lit 

C      KJIC 

Tf  Tt 

^i     *     >* 

I 

CM 

o 

! 

:  6  c 

tpit 

CO         i         i 
1-H     cc     t- 

1 

c3 

CO     tN 

-;  ^^ 

•6  c 

6    6    6 

o 

ft 

c 

6    c 

A    && 

*    ftiz 

ft  ft  ft 

ft' 

03 
60 

.s 

03 

!2 

ft   ^ 

'       co  a 

(/T    vT    y 

' 

"PI 

'£    '^    1 

fr' 

0. 

03       0. 

S  '^'c 

53  a 

03      03      03 

C3     S 

1  ss 

^m 

^   tJ    k5 

S 

W 

PC 

PQ    PC 

^  S£ 

H^h- 

Ks'     K^ 

Hs" 

>> 

§ 

ft 

1 

C3 

o 
■— 

O 

cq 

"8 

o 

el 

2 

ft 

03 

1 

0 
be 
►a 

i 

_c 

2   c 

d    c 

C 

o 

c 

d    o 

c 

ft 

o 

0 

2  22 

'S 

!E 

!a  2 

22 

,3      ^3      ^ 

PC 

CO 

c 

o  o 

o  oo 

oo 

O  O  O 

CO 

TJ, 

IS 

O     I> 

fl     CIM 

i-ICN 

CO     ^     IO 

ft  • 

03  O 

Sft 

a 
o   . 

33  © 

H 

H 

m 

<>ft 

ft 

a'i 

i* 

co 

1 

i 

lO 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


285 


— 
- 
0 

c 
- 

c 

a 

e 

X 

JZ 
r 

I 

"3 

3 

C3 

2 
a 
'So 

x\ 
o 

a 

_o 

o 

rd 

c 
t-, 

PH 

<u 

PQ 

s 
0 

■- 

r 

a 
a 

— 

ill 

fA 

111 

0Q0Q<-! 

8 

o 

i 

■a 

<N 

o 
c 

oo 

oo 
cct- 

esi 

0 

o 

co  io 

93  OS 

^ 

at 

_?  ■ 

o 

o 

o 
o 

o 

8 

1 

OJ 

a 
5 

co 
re 

O 

pi 

3 

CO  CM 

oo 

m  o 

<MO 
O  •«" 

^ 

8 

OS 

EG 

I  - 
M 

o 

OS 

a 

s 

X 

OS 

o  ic 
So 

2gfe 

os  co  oo 

s 

-rpr^cDO-H^-^aO-^cooo 
rt^iOi-i'-ioooroNO 

NOffi'T'CiCOiNHfflC^^OC-XKCCCCCCCCiOiHfqNOONOOr-CCCCrtCOHNX 
-<^OOiOrH^Hi-iOOi-iO>-iOOiO^Hi-i>-iO»-iO'-iOi-iOi-iO^<MT-i^HOi-HOO«5tOi-HC> 

316 

323 
414 
324 
399 
409 
426 
932 
1,116 
294 
402 

0!DNHOINNNTt<NN(NlOlOOiH!ON(0<OTfNOlOWOCCCOfOO)NrtNOiOOC(DINP5tO 
NOOlCHOr>OCCCaoOtDOO)1"HOO)0©OOHfflOCl»NO)0)NHXCN»:'KOOONH 
COCOTT'OOOCOCOCCM<^CO^CO^^OCOCOCO^CO^CO^CO^CO^COC<ICOer:OOCO^'*OOOOCO»ft 

00OOOIOM 
CO'*^        CO 

oocoo 
en 

OO^iOOWOtO      ■lOOWiOOOOiONKOO 

(DW^MWOiOWtDM       • 
T1  CO  CO  -V  i-H  CO.        «5  CO  CO      • 

(NOOOlO 
CO          H  tN 

00  IC  lO  O  iC  lO  tD  CO  N  N  O 
-jOC!C>rHOOO)(NCNHOOO> 
Nf-00  0OCO00O)'TfflN0C 

lOOHiflOWiCONOOOOOWfflHNlOifiNOOi'SCNHaiOOOOINCMNiSOCNL'; 
«01»nOOOKNCOfO©ONOO-.HNO©HOOONINa)HOmCNN©Tf«001'« 

oor~ooocor~cooooooocioooocooccooooooocco}oooooc»oooooocooooococoooo 

c 
c 

g 

X 

'u 
PQ 

P 

HP 

© 
g  S 
x 

PQ 

1 

c 
X 

e 
z 

<L 
0 
X 

X 

pq 

pi 

hp 

jt 
2 
£ 

V 

c 
c 

i 

^ 
C 

c 
c 

£ 
5 

> 

r 
;- 

DC 

C 
P 

c 
B 

'~ 

"C 

pc 

P 

c 
UP 

.  ~ 

X\ 

£ 

) 

c 

s 

3 

0 

p 

f. 
0 

p 

6 

PQ 

M 

c 

Hp 

a 

: 

£ 

c 

0 

5 
p 

s 

.2 
T 

pa 

1 

0. 

.  t 

T 
PC 

c 

h: 

a 

J  t 

pc 

-1- 

c 

tp 

J  t 

pE 

c 

<p 

t 
J 

T 

PC 

e 
<Z 
a 

J  s 
PC 

1 

i. 
t 
X 
'■- 

PC 

— 

c 
up 
a 

- 1 
X 

£ 

c 

HP 

c 

i 

i 

c 

C 

c 

- 
O 

c 

1 

I 

1 
hP 

b 

pc 

r- 

HP 

t 
C 
T 
'E 

PC 

1 

IiP 

a. 
; 

2 

PQ 

1 
HP 

ec 

t 

5 

PC 

p 

i 

c 
; 

— i 

(. 
o 

HP 

: 
T 

PQ 

c 

HP 

c 

t 

X 
X 

PQ 

.  - 
.  c 

H    ■  P 
■  c 
.  6 

:pc 

c 
HP 

- 
- 
-r 

PC 

p 

i 

c 
t 
-c 
"E 

c 

HP 

c 

t 

i 

HP 
c_ 

t 

t; 
PC 

C 
HP 

c 

£ 

M 

C 

HP 

a 
.  t 
X 

X 

zz 

-V 

K 

C3 

o  o 

ftp, 

bfl  So 

TJ-O  C 

■cut 

PQCQ 

r 
C3 

!r-<ep 

>rt  si  (i 
o  o  O 
o  ftft 

>.   ©  <D 
f»    t/}6j0 

£•2  "2 

WCCPQ 

l^     OO        00        o 


<N       ?3 


00      N      N 


o- 

EC 

If 

CO 

rt 

o 

O 

c 

c  o 

o 

o 

O 

z 

2-- 

!z 

^7 

■/ 

V 

yx 

. 

■r 

■s. 

99 

a 

i 

S  C3 

t 

t 

p 

2 

£ 

g 

££ 

2 

- 

h4 

^5 

^i 

rt 

^^ 

h,      ,_;      ^3    W      K    K!K 


a    a 
*©   *s 


o      o      o      o 

^   ^   ^   ^ 


o    o      c 


6      6 


2,         —         Z.      —        — 


o     ©    S3    S 


W   Fa     H 
o  o  S  S    s 


o  o 


o    c      c      c    o 


c  c 

oc 


oooooooo 

S    2    2    2    2    2    2    2 
ooooooco 


2   ° 

2  2 
o  o 


O       O     o    o    o       o 

2    2  2  2  2    2 
o    o  o  o  o    o 


00         OS      O         ^      CM 


286 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


•spxreq— jonpoad  yetiui 


^98;— q^dap  p3}0  j, 


ha.   " 


£8 


o> 

.2 
"S 

o 
O 

I 
IS 

CO 

O 


•laej— iflcfep  no 


ran^p  OAoq^  apn^v 


•;89J— I8A8J 

B9S   Avcqaq   apn^i^V 


"*88J— 

parej^euad  ssanjptqj, 


laaj— do^  o;  q^dacr 


a 

o     . 
S3  o 

02 


XMWNMXOSfflOftOI 


KOSC^MfflpHOr.NWI 


i6003c»0©cSC^s©00»e»^NOO^©aOC^W©SCT>dOOT^cO^<b< 

OClOO>HOOOlDHOOOifliOMH,*KHOCMH9HOJCOOOi 


HrtfflHHHMlSONCOHOOLONHlCfflHOfCCHOINntnM' 


NONMNhOMh      .O      •KIDNOOCOOWOWOHIM 
CNCNi-iCNCNCNCNCOCN      •  CN      •  1-1        hOSMhiOiSmhcCWh 


KOWCCCChNl-hINOCOIOC 


'  iO  th  CO  CO  ' 


ifJONMOiO 
NMOOKIINH 


OM^ifliOONcOMNOinNWCOO'-'IOlOfOSiSMCO 

IflHMOCOI'COWOOONtCOHHlOrtHHHHOHHlNO 

H'*oco>o>M'*f(oooictoff.o3'*®xo(xoo)a)OiO!ooo5 


o  o  o 

PhPhPh 
03  03  03 
6CCuD  M 

t3  'CO' 


o  o 

ftp. 


HNCO 

-a  ui  ^  fcj 
5000 

>  «  a)  a: 


^  ft 


.  »rt  k^  »i  «-  t-  *-■  >- 
,  C  T'O  o  o  o  o 

(ft 


i  S>  S  tA  ^  5i)  Sii  SfM  t£    !  ,2  Si  aV,2  Sji^^uiMtxwiboi    • 

O  tJ  t3  e?  r*  "3  "d  t3  <S  ^  Onx)  int  o-^o'CTJ'CO'd  o  O 


:wpc 


2    S 


O      O      CO      IO  Tf<      CO 

S5  S  S  SS  S~ 


o    00 1^  1^  t^  00  oc 


000 
fc     £     55 


w    w    w    w 

0000 

§   a   a   a 


OOO  005  © 

fc  55  53  &•■:  « 

..  ~  ~  ~o  o 

,3  ^j  A  ^a-z  >z 

VI  VI  VI  OlH  M 

03  03  03  03      „  ., 

•_  S-.  U  h   h  J_ 

5  S  5  3  o  03 

o  o  o  o  5  5 

a  a  a  ao  o 


o    000000 

5?  ^z^^^z 


03  C3    03   03   03    03    03 

o  o  o  o  o  o  o 

o  o  o  o  o  o  o 

O  OOOOOP 


o 

c 

c 

3 
o 

o 

3 

o 

O 

3 

o 

o 

o 

O      O      ©      OOO 

3  3  3  33  3 

O   O  O  CO  o 

o 

3 
c 

O 

3 
o 

2  2  2  2  2  9 

3  3  3  3  3  3 

oooooo 

S 

m 

CO 

t^ 

OC 

©     ©     -*     CM  CO     -r 
r-t     <M     <N     CN  <M     CN 

■ri 

-- 

(TO 

CN 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


287 


CO 

z 


£g 


ioctc 


ilC  CO  <-i  CO 


5.5 


°  12 
x  oa 


TiocNinoio 

©  00  ©  00  00  00  © 


SO>iO 
CD  >* 

•-H  ©  © 


©  <M  t  us  lo  cm  r-  ©  <M  -_r  c-.  —  cm  u:  i  --  cm  vr  -r  i  -  i^  ro  —  t~  OB  C  i-  *r  r~  —<  ©  cm  us  u:  re  u-  ©  01  us  ^ 

N  CO  N  N  -  '/  C.  C^  N  W  t-  w  C  N  (N  X  ^  I-  '-  ff.  ?■  -i  T  ^  X  -H  r-  5  OC  C  N  N  N  X  f-  rt  Ll  p  C  C,  C 


I  O  »-H  rt  f-H  t~-  .-H  O  1 


llOl-H  Ohh 


C  N  C-l  r-  C  M 
_  C  X  O  X  N  Oi 

©—l©T-l,-l,-l,—  —(©© 


iMffliOiOXMOXiTH 
©  CO  CM  30  ^h  O  30  C-  l^  CM 

>T©CMCMcececoeoTr>ee 


tXic  r-  y_  t  a  «  k  t^  c  re  fh  c  k  •-  re  S".  —  x  -e  us  i~  ^rxifloiooc  00  00  a:  t  00 
•/::rn--c?ir:cCr:i-r:?)XXC'HccN(NNHMX')'Oroc«iJ''HKH«o 
ce-^^cerecoco^ce^^co^cocecer~co^co©co^iroeeco^co^.ocoeococo^^ 


0!Oi^nt-ooNrrooNct-iM-r:y.c^r.'-c/.cr.^C-  x  r  i-cwccci-ccncickjocm 
x  now  n  --  n  t  «  rr  x  1-  c  x  -  1-  n  /  r.  /  /  c  n  c  r.  ■:  •;  /.  c  rt  re  in  c  c.  n  f-  tt  c-  n  -  t  n  c-  n  c  c  o. 

©©TTt^l^CCI^00CO©l^Cf_CCX00l^CGI>CCr^0O©0COCt>-0000i^C>0©00^CC00CCO0OCOC00©CX;0cr~ajCC©  00 


Cd  o 


.  t-J    k.  fc-    fc.    fc- 

•  O  K?o  °  ° 

.  o-^  PhPhCV 

•  >  o  ®  ®  ®  ' 

J -3  o'C'Ct" 


1  c  c  c  o 

^PhPhPhP, 
'  05  03  05  05 
0  W)  S£  fc£  tC 


,-<  CM  —i  CM  i-«  CM 


<CM,-cCM 


c  o  o  o 

05  05   05   05 


OOOOOO 
P,P,P,P,P,Ph 
05  05  05  05  05  05 
CGCJtcuUCfl     .   t£  t/.  tr,  t£  ti  SX)     >   «/»»»     ._£-w,^w.r     » -~  -»-  »~,  w,  w^  w—  —v     . 

2  2  2 13  °  2  2  2  2  2  2  c  2  2  2  2  °'^222'fc-;222222'c,c2.t:50 
££££  l£££££~  ":££;££  ;popQpQpQWpg(PCQ  ~ 


_  -  _  _ 

fc£  fc£  fcC  &C 


1-lCOl-i        I^NHNH'N'rtKNH 

l_   •—   — —   —   '—   —   fc-i.(_t.t.fc.fcH 
cSCOOcCOOOOOOCOO 

P    P<P<P<C    P-ft1C1P-P,PHP,P,q,P, 
C3O0505>C/fl5OO05OQ5a50505 

«  2  2  2  •£  2  2  2  2  2 


000 

ftp.  p. 

00c 
txtxtx 

tJ'O'C  o 
•    T3 


:~~__.p:«    ipepep: 


a>    nhoooh    00 

Si     OCMNHH     © 
•^1     US  US  US  US  US     US 


t~-        ©        0C        (N     01     Oi 

©         US        ©        ©     ©     US 


cm    ©    r^ 


o  o 

zz 


o  o 

"05    Jsj'g.S'S 


Z         Z 


0 

0 

0 

0 

0 

0 

I? 

£ 

Z 

Z 

z 

Z 

n 

te 

* 

is 

P 

Is 

is 

z  z  z   z 


ZZZZZZZZZZZoo 


CM  -M  |-| 

doc 
Z     Z     Z 


o      o 
Z     Z 


,-1  HH  ,-1     CM 
0666 

zzzz 


z   z  z 


«     Pi     tf 


—  ^^,o 
c  c  c  c 


.S    5  .9 

J2      £l    £i 
OOO 


"3  "3 

05   05 

cn  oe 

05  05 

« 

O 

.Scc.2.2 

c 

O 

0 

c 

0 

c 

c 

c 

c 

z 

O 

O 

c 

0 

c 

0 

c 

0 

c 

0  c  c  0 

0 

c 

0 

3 

^3    05   0^4: 

fl 

— 

A 

& 

- 

— 

Xi 

— 

,P.=  ^,c! 

& 

2 

- 

0 

oKScc 

0 

O 

c 

C 

O 

O 

Z 

0 

0 

0 

C 

O 

0 

0 

0 

0 

c 

Z 

0 

oocc 

a 

0 

0 

© 

t^  0C  C5  ©  — 

N 

CO 

© 

t^ 

X 

© 

§ 

CM 

CM 

S 

c. 

fcQ 

§ 

1  - 

c-i 

-N 

CO 

TL3CN 

X 

0. 

a 

288 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


lO  "5  CO< 


•s{8JjBq— }onpojd  i^prai 


•199J- tfldep  ib^o  j, 


to  LO  lO  CO 


•laaj— ittdap  no 


<N  O  O  CO 


tnrn'Bp  OAoqe  epn^^Y 


Tf  t-  CO  GC  00  CO 


OC  COCO  iC  COi 


•!}88J— I9A8I 

■Gas    Avojaq    aprni^xv 


(M  co  cc  < 
co  t  co  co ' 


l!5NNOO>00<00 


i  o      Hosoao 

<  CO  CO  -f  -«J<  TJt        CO  TT- CO  CO  lO 


I  COT  00  O) 


188J— 

pa^aiairad  ssaajppij; 


I  U5  C  CO  >C  tN  CO  tN  I 


CNlOrHCNCC  i 


I  lO  CO  CO  CO 


•598J— do^  01  Tftd9(I 


HNOiO. 
00  Ci  00  00  Oi  < 


)  as  oo  oi  a>  CT>  oo 


OOMMOW 
-r  CO  (M  CO  CN  CO 
00  05000  050 


swNoiomN 


ooo    .ooooo 

P<P,P4      .ftftP.ftP, 
CD   CD   CD      .   CD   CD   CD   CD   CD 

be  be  6X)    .  bJD  be  b£  b/)  be 

'C  "fi  'C  ^  "C  "C  '£  "d  -C  ^  *c  'C 

eqpqpq    '.capqpqpqcQ    :   :po 


-   J  p   . 

i-iCMCOi-HCNeO  03  p- 

4^  4!=  ■*!>  -i  -m  J>  -u  c3 

!_S-,tJt_t-,fc.fc.rH 

ooooooog 

ft  Oh  p.  ft  P,  p,  ft  2 

CP   CD   CD   CD   ©  CD   CD-^S      ►> 

3  si 


.Jo  <d : 


o 
b/,  bX)b£>bJDbOb£bJ0$J  OT  R  CD  .2  be  be  w  R 

pqpopQpepqpqpq    3  ^^SflBiW 


£  Si  c3  p"g 


10     10  10  Tfi 


TJ" 

i-H 

tc 

00 

0 

«-ti-<  1-1 

0 

c 

A 

O 
ft 

0 
ft 

0 

ft 

0 
ft 

000 
ftftft 

ft 

in 

3 

cr" 

pj 

c/T 

P 

wT  c/T  to" 

p  p  g 

a 

O 

■8 

P3 

A 
A 
0 

.  0 

■5 

000 

B 
s 
0 

Sft 


,P 

A 

£ 

fl 

fl 

AA 

£ 

2 

a 

a 

O 

C 

O 

c 

c 

000 

TJ1 

CO 

CO 

C] 

ea 

>' 

cor- 

CO 

(M 

CO 

BLATCHLEY] 


TABLES   OF   WELL   DATA. 


289 


li 


08  <" 


g  3 

pc2 


19 

fcT«-T 

d  el 


o  o 
;toto 


o      o 

TO       TO 


ia.o>     Tif-.o»o»t»^,05'^'- 


iooooco      ooooimwochn      r^      »0C!CNinNtot^tCHXHC*O)Xioci0M«iotNNo>eci 

1 .-«  ©  O        0«!OiOOt«NH        O       ^tOCCiO^MHOOHOOOOiOOOOOOCXNfDOiOiCM 


i<o«i  -^  Hp-HtoNrtioooocoxMmooooNrroie'.ei'^pKOioo 
loriM  cn»  OHt<5iN'<i>Nco«'*cr.'Hwo«OiHTiir-a5rHi'io<siNOMO 
i  cs  co      -«r      r-  oc  oo  OS  a>  o  >-h  co  tj<  -n"  oo  •*)«  cc  oo  e»  -a"  ■«<  i- t>  co  «c  i~-  oc  oo  as  o  ^* 


OUTOO        >ONOONiOO«iO        O        00©0<^©-^COOOOOOiO<OOOiOiO>-0  0>OCB>OiO>n 
- >  CO  OC  0C        HHiONt^MMOf        "I<        NWfl^C^iOiOCrt'fl'i-iolffiKMCKa.  «CN<irKNiON 
"■1»'T1no©XOO»C«f  — 


t^OOOJOi       ONCOffiOi 


1 00       Ol        CM  COt 


iOOlfflHH«MWt^(D 


TOS 


•--hCM 

•  o  o 

•  o  o 

55 


^i  iJ   (D   fl)   G3  i 


2  oo  So  So 


cj  c3 

P5k 


•  <d*d 

.  o  o 

•  O  O  . 


;    ;  ^-i  cn  co  i-H  op 

•     .  -u  -Ja  -ti>  -*i>  -i 

.  K^  t-l  fc.  «-  i~  (~ 
.  p?o  o  o  o  o 

geooo© 


rrj  fc-  fc.  *- 

5000 
o  Pt^ft 

P  P 


e?££o 


bo 

bo 

g 

bo 
1 

i 

1 

a 

•6 

a 

a 

a 

a 

a 

3 

3 

3 

O 

0 

0 

0 

m 

m 

m 

fl 

g 

a 

3 

0 

0J 

e 

s 

© 

•d 

•0 

•d 

•d 

1 

k 

0 

K 

a 

a 

a- 

3 

OQ 

02 

TO 

TO 

—19  G 


290 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•  spire  q— pnpoid  repux 


%Qdi— q;dap  rejoj, 


•J88J— qidap  po 


0 

■  r-C 
Pi 

o 

t 


a: 


•J98j— eu^id 
ran:rep  aAoq'B  gpnmjv 


•}88J— I8A8I 

■ess   -Aiopq   apnji^v 


pa^xianad  ssanjpiqj, 


■%Zdj— do;  oj  qidaa 


=  o  ©  c3  C"S 
02<S2  ©  >££> 


■*i  -^r1  as  -^f  o  o 


I  S,  O  O  iO 

(NCDCOIN 
i  Tf  if  lO  O 


OC05fflOCX05  020rHCO 


■Cd 


:c3    i 


C    B 
O   0 


§1 


o  o  o  o 

<D  ©  ft)  © 

tt  SJO  6i)  W) 


J=!  b<2 


'd  C*dxi  O  O  O-?  o3  03 


I  CO  O  1-H  CO  'SI  CO  CO  CO  O  (0!OH©HHO)(D010  OC  T-A  I 

•  t--  CN         NOOCCMrHN         C>.UOH00ClNONNin         O^fl 
lOO       Oi  OC  »C  iO  iO  •"*>  00       hOOhhOOOOCO       to  W  < 


H^rtO  CM  C5  Tf 

as  <n  r—  ic     oi  «o  t-» 


io  >-o  r~  t~  io  co  co      oot^oo®cf.inicN     t^ 

•f  <N  00        IN^HMHWNCNrttN 


•ss 


^£  o 

03^0 
im  S  o 

SMS 


sz 


BLATCHLET] 


TABLES    OF    WELL    DATA. 


291 


C 

9 

o 

CO 

o 
a 

a 

c 

cc 

8 

0 

\r.  i  - 

a  c 

OO  CM 

—  i  - 

©  9 
tit 

x  55 

1 

3 
« 

D 

0 

' 

© 

— 

--0 

CO    c 

a  a 
id  a 

sfs 

i. 
c 

8 

t 

0C 

«■- 

8 

e 

c 
a 

0 

C3 

I*  : 

•  -w  • 
;  ©  : 

•  «2    • 

sal 

<S^c3 
OcC 

c 
c. 

c 
C 

©    • 
©    • 

co  C 
o  o 
i-T-rJ 

tS 

©,q 
CO 

© 

c3 

C 

1*2 

3 

OO 

coco 

OOO 

oo  r~  >o 

IO  O  X3  LO  W  U5 

IO  iO 

IO 

CO 

o 

lOO 

ooo 

OOOiOO 

N  «  IO  tO  ■* 

S 

OC 

M 

00 

o 

LO  CO 

oo  o 

OO 

3££ 

MOOl 

CXI  -p  ^  <M  o 
Tf  <N  0C  CO  Tfl 
t~  TP  -*  iO  iO 

00 

OOO 

00  GO 

r~o 

oc 

CM  OC 
t^00 
OO 

cecCNMN 
O  00  O  00  i-l 
OO  O  IO  CO 

o 

00 

SO 

00 

kO        iO 

r-      r~ 

oo      o 

uo 

o 
o 

00OO 
OOO 
O  COO 

woooram 

OHMi-iWM 

t-  t*<  t)<  io  »o  »o 

t-o 

lO 

'0O 

§8 
oo 

I-~  i-H  i-H  Tt>  00 
OOOiOlO 

! 

CO 

C 

r: 
CC 

co 

-r 
CO 

•a 

re 

CM 

o 

3 
— 

SO 
IO 

o 

co 

HNNO)00>«iOOOOCOO©Om 

MiOiOCO»HNNONMr-IMHN'* 
WHOOiOMOOiOMOOiOiOiQN 

!»C*iOXrHOCOCOOO 

■vNoioMHNecco 

OlONOliCOWW 

lOnooio^HO 

-*- 

CM 

!>.        I>.        t-.t^tOr-OOOTtiTl<COMCO 
IO        IO        IO  CN  CO  IO  -eft  tO  CM  lO  O  CO  ■** 

co      f      oo  o  o  o  ■*  co  o  »-i  >-h  eo -"cr* 


(NiOOOONO^ONHS^XOOLltOOCOOO 
NNOXl-MNOOOOLCTHCUC'WHQONMfflH 
OOVOHOOOOOOJOlNOlN^OlWWOlOOH'* 


>H^^O)OCO,11 


iO  CM 


IO  CO  00  lO  rj*      •  iO  lO  r- O  iO  o  < 
H         HHIN      •  (M  i-H  CM  "*  < 


>  O  CM  iO  lO  o      ■  O  CM  CO  O  "*r  O  CM  O  O  iO  O  »0  CM  O  CO 
ICMMCCHih      •  <N  <N  <N  CO  i-l  CM  r-H  CM  CM  i-H  i-H  CO  i-H        r- 


lO»O-<»<<OCM-*0000C0lO>Oi-(< 


oo      O      ec*' 


. .    JCOlOlOHOHiOOOOVONlOONINONMMlOiJ'OOOOlO         IO  O  i-H  O 
-•t>'»M5*iO*iOOIlCVNOOMOC,lMOrOrrti-TNNHNL')H         NNHH..  . 
0>W*ffl!OMO)0>1"tOMCii.'3t»*TtiiOiQC(10iONO)VN»*M!0  0        -fOOOiOiOOOO 


NN        OC  lO 


bog 
©  ©^ 

(-1  s-, " 

pee 


i  o  o 
i  o  o 


'CM 


>/S   >■ 


MMMPQ 


O-ou'C'S'O-hoO'C'hcO'O 


:§WScst>^pcw-  Spq 


orT'2    •  o    "22      o  P 

b.5!;©     .►>     •  CD  ©        fe-g 

M§pq   :m  :pqpq    WS 


■f       CM     O    O    CO  iO    O    Tti  co  co  i-H 

CN  i-H       ^H       i-H       ^H  rt       CM       CO^fCOXtl 

iO        IO     C     io     1310     13     ttJiOOiO 


S        CM 


IO         lO     lO     lO 


■ViOiO     lO 


iO 
1^     O     r-1 

6      O      O  MN  Oi  HTfiOC 

£i(Zi!z;  qq  q  6666  o 

CO      CO  p     »■  -  js     J.    «     •<  -. 

H  C  C  i  •»  I  C  i  i- 

■-"^•-;«2<S  °  °°2°  £ 

K  H  w  J513  'd  'S'5'5'5  t3 

£    o    O  CD©  ©  ©©©©  © 

SSS  cops  cc  ccpsp:pq  PQ 


©   © 


^  fc 


*2     bB    b3 


o    o 


o  oh 


55  z^;^ 


tjO 


Pi 

S  £  M    S 

© 

ca  H-;  i-i    ,-,• 


M  M 


biB    bcbcQ  _r  .? 

fl    fl  p|  g  g  g 

M MMS >  > 

.     .  E3  ©  © 


d 
cc 

0 

^3 

O 

O 

c 

C 

OO 

Z 

OOOO 

c 

0 

O 

"a 

c 

A 
C 

0 

OOOO 

A 

0 

0 

CO 

10 

to 

X 

0  0 

i-H  CN 

CM 

CM  (N<M  CS 

S 

C~l 

CM 

R 

0 

re 

M 

CO 

CO 

f  iO!Dl^ 
CO  CO  CO  CO 

00 
CO 

2* 

CO 

292 


OIL  FIELDS  OF  CRAWFORD  AXD  LAWRENCE  COUNTIES,    [bull.  no.  22 


;  os  os 


©  ©  © 
©  ©£££ 


igas 


©o©fi;o 
OS  C3  C-  C3  & 


I'a   :*3'S"3"e5'c3 
\m    .cocccococo 


©  ©S 

eS'S'S 

rococo 


•spireq— icmpojd  ibijiui 


•:*99j— qjdgp  [Bjo j, 


S3 


•laaj— qjdap  no 


sssss 


^8 


o 

I 

3 


c 

n 


199j — quv\& 
umiBp  8AoqB  oprnpiY 


'Nkl-:  --  x  ■-  ~  ~  —  -j  —  ■-.  o  —  m tj. •— 


-HM'VNMi 


ss 


-r  t  cr.  i^  r>-  r~ 


B3S    Avopq    epnmiv 


ts  x  w  o  t^  c  i-  i-  l-  r.  z  x  •-■:  i>  cm  mn  in  cc  tt  -  c.  !•■  o  m  e  tc  r-  «  «  n  » 

KOONC-^-^CC/.l-C-C'.X-rL-L'.rNONCXICNPlNf.O 

ooHOCocTCCfcicNns^ccn^ioNocccoiOKioow 


•J99J— 

p9^BJi8U9d  ssgu^orqj, 


OCT? 


SiSSS8sag5^SgSgSS8SSS3e-5gjJ 


•^99;— doj  oi  mdacr 


^^  ^v  w3  ^,  I>-  IT5  T  I 


u-;  X  X  CM  00  •"r  L.C  X  C  ■ 


■o^woei 


£  ° 


©£ 
2*9 


o  P< 
>  © 


c  a   ■  o  co.o.a 


:§.S 


.=  .«=  >> 


!mM 


^  "C  i  •-  n  *o  a  s^ittu  s  c  is  •-  ^  c  shi^ 
:ero^-  :capQmMnpQPQ«?  co^  iceS^  : 


rn  g  ©  >   3  .© 


o        10 


CM     CO     lO 

6    6    6 


CO     £         ^ 


a  «  ^  -.    - 

O  C  C  G     fl 


O    O    OcococO    CO 


S£ 


I     8 

Ch       ft, 

ti     to 


o    o    occc    o  ^ 

o  o  0000  o  a 


«  n 

•3  « 

O  O  "2 

co  co       O 


~) 


cc        ■*• 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


293 


o    o 


b  o 
CO 


uO  O  O  O  O  O  O  ' 


OOONMOOOOl 


cor^i-ic^occo 


c  o 

(Ni-h" 


rlOCWMiOOOCCOiN'O'M 
NHOKNHirHrtfflLO 
10K30)0>0!0"150)OON 


OONCt^HCON'^Oli.lMHOH' 
OcOtOi-CT.- IC0I^cNO.-<t-O-J<l 


■fcococoeO'^n'V'J'O'^'t--' 


N  O  O  O  N  9D  IS  O         HO-HOKNOOHOi 


£J£JiO        OOMOOOiqiOaiHOOO« 

SCXCf         O-r-C0C0l^l0c0i-ie0C0'«?<'<I« 


CN  CO  lO  CO  < 
OCOKOOi 


MOiHlON! 


10)0000  0)1 


OOOOONfflMiON 


oooota      c  o  i~  c-i  c  ic  ic  i—  c--  ci  c  - 


OHOHNiOtOtON 


o  n  o  ^  n  m  f:  n  -  a  c  m  r-  c-  x  in  r  x  a.  n  to  l-.  x  n      OKOLiocorKia 

O  M  lO  X  t-  -  X  C  O  D  O.  C  h  X  I  -  -  h  T  C  r:  i.-  t  N  X         C.OOp-fjMOCON 

to  so  o  c  c  c  10  l-  c  c  ^  >.-:  c  -  c.  -  x  l:  -  -  c  t-  c  f.      tNocfjMOcooojo 


COiOOCOtNcCWt^iOiOirj! 


.2  °  ° 


o  o  o  o 

'3'3'3  T3 


•  2  c 
'  6*° 

CO* 


i  un3  .  (-. 

,  O  o  •  ° 

i  fto  ■  ft 

1  ®  > 


►>.  co  ir  ot 


K-        *    CJU      *    CJU  *^       *    CUU      •    si' 

.h  ts -r"c3 -r  .a  •«  t- t3  ™ 


3.3*3 -cot:.-. 


"3 


•3   3*3 

c  s  o 


•  O  C3  _  . 

o  q  o  3  o 
-£2>2> 


•O'd'd  g  3*3  >*3 

o  o  c  q  q  0>*a  o 


".Enawa    cnweccc  :^£^£^ 


3*C3 

fa   :W 


'«  :  •     'win 

■  c  c 

^&^?c;  ill 
ISsSlf*§:§.§:s:8 


cr.  ih  cn  n  cc    co 


o    io  ic  c  lo  k;  io  v  ■ 


2    S    8  S8 

m      io      io    ic  m 


>7 

o  o  o  O  o^1    o 

Jfcfcfcfcfc,?  55 

C  O  S  O  51  «  CS     o> 

**§<&&&§<&  & 

ggoooooW O 
^■g ^ 


CN  CN  CN  i-i  i-i  CO  Oi 


X      OOOOOOOO      O 
O      b£  be  ho  b£  tA  bC  bC  bC     bo 

.   cocpchcc   q 

» QQmmmmSm m 

2    H-s  h-J  1-^  H-s'  >->'  l-s'  1-9  1-j     (-»' 


55     fc 


55  £ 

I^§  § 

M   g§  § 

•   m  ,« 

*    5  3  s 

k,-  ^ca  CO 


Pi  c 


O    r«  bio  E 


.2.2  2  2  2  2  2  2  .2  2°  22  2  2  2  2  2  2  2 

3 3 2 2 £'.2 £2  2  2  2£££££££  £    £ 

oooooooo  o  o  ocooocoo  o    o 

lOtOrtNCO^riCiH     CN  CO     ■ffCet^XOiOw     CN        CO 


3     3  3 

o    o  o 

£    £    £    £    £  'S.Sf  if  if    £  £ 

ooocefs-ja  -oo 


o    o 


CN         CO 


u-5     Ot^     00 


O      f-H 


E 

© 

5  I 
.1  & 

o    o.3  fca 

£  £s  ,§ 

o  o<:  a 

C*     — iCN     CO 


294 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spjJBq— prtpojcl  i^puj 


•;89j— mdsp  p^oj, 


•loaj— q^dap  no 


a 

•  I-H 
PS 

o 
O 

1 

8 


•^98]— 8UB^d 

ran},ep  8AoqB  aprnxiqy 


•J88J— \QAQ\ 

Avopq    apnjiqy 


•}99J— 

pa^jiauod  ssau^oxqj, 


!j88j— do;  <n  q^daa 


iL  a>   i     i     I  jJ 

5  o  a>  c3  fl  « 

to<2  ©  >.2<£ 


I 

ft    • 
b3  O 

2* 


o    . 

GO 


COMNINOHTtlO'l'rHMNl-ll^lOrHOOrHOfOllNtOINlOINNNNC.'fOI 
^^CO^CO^CO^P5C<5CaCOOOC^<N<NCOCO<Ni--l'^icOCOC^'^irOCOC5CCCOC<3l 


iOIN»tONr-m'WOOMlOCOiOtONOTl'CCIN'>}.N(OCfc'<I'0«OlOeiflN 

iNOHrtWHHnN 


00>iOCOl^lOi-liCi-<i-iTMOCOiOCDl^-0-^'<C<MOOO!NTrCOaJOOOOi-iOC<l 

O'^HlOIMtDCOtDWlCCOOOtCfjO-rOU'rNtDCDNtOCCffl'-KMMOlCOH 


(M  . 


I  CNrH 

o  o  o 
o  o  o 
£££ 

323 www 35 


o  o  o 


o  o 
o  o 


^•OTJ 


l>v^w^         OOO     •  O  O 
-.'SOOO'OOO'OO 

fe.  >>^  ££>■>( 


£    55    £ 


£    £ 


1-3    ^ 


2    OQ 

I  «8 


PI 

fl 

fl 

a 

a 

o 

o 

o 

o 

o 

cfl 

OQ 

cc 

XII 

ou 

°a 

=3 

•a 

°3 

■a 

CO 

c- 

D 

P 

o 

o 

O 

o 

o 

rC 

£ 

A 

$ 

JZ 

«4 

«< 

< 

*d 

< 

BLATCHLEY] 


TABLES    OF    WELL   DATA. 


295 


°£ 


«2fe.£ 
» teg 
a>  £00 


CcoCJ 


;o  cm  t>  c  co 


o  m  o  o 

CM  t-i  CO  O 


(CiQMCC 


£8 

COO 


ST.  ^H  Oi  l~-  00 

oo  o>  oo  oo  oo 


fOWM 
00  OO  00  00 
00  00  00  00 


m  oc  oo  io 


iOCNcomcOOO-<rCMinr--COCO-*'T^H        00  v  00  io  t»  t  N  T  ff.  f  UC  W  *  r 

cocoocococNcoeococMcococoCMCM      c-*OT-ioo>-HOmioi-tooocoo 


ifl'fl'OCOl' 


OOOOOt-OOOGGOi-hOcCi 


Tfco^^^-vSrococoin 


CM        -V  CO  T  CO  • 


i  Os  co  -*r  -*r  ^n  oo  -f 


|eo^f^P'«i""<3iTr,^cO' 


oc  a  ■f'T  <» 


l«  CM  00  •'9' 00  O  CM  CM  00  CO  CN  CO  i— I  CM  CM        CNO^ON      •  CO  00  T  IO  CC  IO      •  OS  O  OS  < 
rtT^^H        i-ii-Hi-l  Hi-iriHrt       N^Crt      •  -«3i  CM  CO  CN  CO  CM      •  CN  CO  CN  ( 


OONCNtOOCNlMMtflCNiOCflTHOOO 

•^t^M'Tnr-NinN-wc>0CN>O'*c<5t^ 

COCOO>COCOt>COCOCOt>COCOCOr~t>- 


lO  O  ON  N  00  00 

OOMCSNOJHOOOXT 

000C00O00CO500CT>CO^ 


ONCDMl-OMOJ 


00  00  ON  CO  C  tO  CO  " 


ia  co  oo  coo 


O  m  O  > 


o  o  o  o  o 


■d'd'd 
o  o  o 


w  ^  —  w  w     -  w  w  1-* 

o  o  fto  o    •  o  o  o 


o  o  o 
o  o  o 


OOrtOO.'OOO.'OOO' 
M^^MM    O^^i^    O^^^i    CJ 

t_  ^  — .  (-it-c3tHS-^c3>-itjJ-c3 


SSS55 
ftp,  ftp.  ft 

©  a-  «  <v  © 

bX)  bO  be  b0  bT. 


c  o 

ftft^ 


o  o  loo 

,       O  ft  •  ftft  r 

CD   CBJ      fe-  ©  •  ©  ©2  © 

b0  60  <y.    l>  bO  .    60  bT  r^  b0 


bX)  bo  bo  60  br.    .  bo  bo  cr,  >  bo    .  bo  bj'  ~  b/ 
•CP'P'P'P  CCP  cS^'P  O'd'd  03 TJ 

t3  "C  "C  "C  "C  "ti'C'Co  rt  "c  ^'S'Co  "fi 
pqpqp^pQpq  :mpc;  ^im  :pcm-  pa 


o  o  o    . 
ftftft  • 

CD   ©  ©      . 
bobobc    . 

tiooo  COtCti  o 
'C'd'd'd'd'C'C'C'c) 

pa  :  :  :  ipapapq  : 


r-CN 

2  2  § 


tx  60. 

'O  o  cd'd 

pa  :  : pc pope 


°  2 

o  ft 
tfc  * 
^•o  o  o 

Wpq  :  : 


5  § 


■f    OS       <*    N    t* 

r-   r-     n    to    io 


CO     rH     i-H  00  rji  f-  CO 

m    f-    t^coemio 


loco     CO 


Ol       T-l  i-H  i-H  1-1 


o    o 

o 

o 

o 

fc  £#£ 

fc 

1? 

w 

wi 

rr 

M  tt 

w 

w 

w 

p   p 

p 

p 

p 

03     c3 

03 

03 

p   p 

P 

§ 

p 

03     03 

C3 

03 

.p  ,p 

■P 

,P 

,P 

o 

p    p 

p 

3 

P 

pa  ca 

PC 

PC 

- 

co    co      cm    m 


§8  fc    £  £    £  £  £    £ 


O    O    o    ccooooo 


CM         CO     CO  ' 


o    o  o  o    o 


CO     ION  CO 


o    o  o  o 


o    o 


p    p 


o    o    ooooooo    o 

po  p  cc  ps  pc  pc  pa  pa  pa  pa 


g  888  8 

o    o  c  o    o 

pa  papapa  pa 


&4     PM        ft,  pt!        Pm 


ooooooo 


PQ    25 

« 

S 

55 

o 

c  o 

A    A 
O    O 

AAA 
COO 

A 
Z 

AAA    AAAAAAA    A 

o  o  o  OOOOOOO  o 

^=    ^^^J    A 

o  ooo  o 

A    AAA 

o  ooo 

■n    co 

t^ 

00 

— 

o 

rt      CM 
CN     CN 

>-l     CN 

CO     -Oi     >c 

CO 

t^    oo    oi    o  —  cm  co  -*1  m  co    t^ 

00-      OlOH      CM 
>-l     i-h  CM  CM     (N 

SJI     CMCMCM 

296 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


881 


88 


ipueq— ^onpoad  ibt^ph 


•;aaj— ttfdop  ib^oj, 


ooo 


•;aaj— q^dap  no 


HO* 

OOOIN 


i 


•aaaj— ouB[d 
ran^p  9AoqB  apti^y 


NXtONOHVHINM' 


rHTfOJOXI 


^tCNOKOXOOCNtOpOtp 


iOO!00(Ou}tOOONU50 


•eas   Mcqaq   aptqptv 


'coTco-<(<Tt<coT'co"<r'Tt<'TnaicoT>Tf< 


I  TJ1  00  05  00  ■<*  TP  t~~  I 


•T99J— 

pa^i^aiiad  ssau^jiqj, 


•^aaj— do;  o%  qidaa; 


_    -<oeoooor^.<_. 

OOOOCTJOlTfiOO  CT.  OCOiOOOSOOOOOOOCOiOOaiTttOOaOOOCNOOCN' 


)  00  OS  lO  IC  < 


fa  O  O  <SJ  fl 


U 


o 

O 

o  o 

a 

o 

o 

o 

"", 

fe 

» 

££ 

& 

5 

fe 

£ 

o 

o 

9? 

03 

M 

03 

rr 

a 

B 

as 

B 

e 

a 

s 

bS 

bE 

rf 

03  C3 

<r> 

ed 

ea 

ed 

J 

a 

g 

g 

BB 

g 

3 

g 

a 

M 

M 

w  CM  i-h     riCN 

52  ...    . 

^  o  o    o  o 

e£  £  £  ££ 

#g  „  ,    .  ^ 

M  o  o    o  o 

^  o  o    o  o 

I-,-  pa  pq  papa 


o  o 


o      o 


as 

g . 

•&  O 
CO 


o    o    o  o    o 

O 

ooo 

o 

o    o 

ooo 

o 

o  o 

i 

1 

A  A  aa  ,=! 

A 

AAA 

rC 

A    A 

A   AA 

A 

AA 

O  O  OO  O 

O 

OOO 

o 

O   O 

O   OO 

O 

OO 

h1 

kJ 

c*5    cn    cnco   co 

CM 

CO 

CO     CO 

BLATCHLEY] 


TABLES   OF   WELL   DATA. 


297 


1 

s 

- 

'I 

— 

1 

s 

■3 

I 

c 

CM 

c 

1 
if 

"ej 

"3 

02 

1 

o 

if 

C3 

1 

- 

c 

s 

0 

I 

c- 

H 

■ 
1 

1 

CO 
1  - 

ft 

cjcc 

=a» 

OQ.C 

:S  : 

.  ox)    . 

■I-<'J-    • 
5?        • 

si: 

co  3    • 

c°  : 

«     • 

"So  J 

GG-h 

:  3  : 

!  °    ! 

©+TO 

33  a 

05*1$ 

aw 

Si 

.P 

CO 

§1 

.p-p 

OQCG 

s 

KJ 

I- 

CM 

OiOCO 

OO    fe 
*CCog 

Jp 
GO 

§ 

0 

a 

CO 

28 

OS 

— ' 
OS 

o 

CO 

S3 

■XI 

CO 
OS 

CB 

CNO-H 

Ci  CO  CO 

00;^ 

core    -oc 

•f  IO      'CO 

Q 

s 

0 
en 

c 
S 

B 

— 

T 
CO 

30 

5 

5 

T 

8 

- 

8S 

O 

o 

— 

CO 

g 

c 

SS8 

CO  CO  ■>* 

C 

c 

re 

•0 

s 

10 

CO 

ioohoomomoomohomohohhohooiohioioo^ooi 


irj  tji  o  <o  t^ 


^occcTj«<»co^^cc^^t^coc>3^^r--coecT»<t>.cocorticoco^co-T<TPCoeococo-^'t^.'j''^1! 


O  —1  1—  00  CO 

OtONCW 
0)0  WN 


is^s  '.ss^^sssss: 


■  w  v  n  w 

'NMHH 


cm      csococm, 


NNOOOOOiOOOOCOSMCOiOOOWOCTliOllNeOiOHOWiOOCOOiniOViOOi 
Ot0wO(DNO1'NO«tHHCNnoOO*HmO00U5OMC<3OtDINHNOHH©! 

cstNmQW«roo)af;OOiN'»,»o>o)NeoMOi«*MO>Nflo»oooi«iTi-eo*Ti«owoo)i 


TTlOGOCOtN 


!  <N  CO  1-1  d  CO  CM  CO  <N      !rH 


-P  3 


o 
cofflCQ 


t-  (_  l_  )_  (_  (_ 

000000 


a»cj  u  t*  t-  p»p  vc  >h  p-p  «-  »h  >-  t-  s-  sh  (-.  t<»p  — 

ft  ft  ft  ft  ft  D,  ft  ft  o 


UUUUUU03OuuuwOuuHOuyuu,JUUUOu        • 

ftftftftftft  p  o  ft  ftft  p  0  ft  ft  p  o  ft  ftftftftftftfto  ft   • 

©CB«5©©«3>©«><»3^a>©c3^-a><»©<i>CPCDCDC»>>  ®~ 

be  60  OX)  60  60  6/jj-i   !>  60  60  DC  3   R   M  S0_3   r.   M  60  be  60  60  60 =0  60  P   60  m     .  60  j-  60  60  h 

S.'S!222So^2.'22o'^.'S2,S'^.'2r2.,2SS.'2S3'£.'203c2'^22'" 

CC  t**C"C"fi  PtH*G  CC  SfH*C"fl  3;-'C'C'C'E'C'C'E'C'H'no^'C  p"CC  3 
P3mpqmPQp5p;Mmp3WWMmp3CO^CQCQpQCQCQp3CQpc!^(a-      :pQCQPOCQW 


OflOO§ 


o  o  g  2  03 

o  o  ftftp 


MM«p2w    Wmeq 


o  o  o 

o  ftft 


tj<     -*n  -V     tji     iO     kO 


0 

cc 

<M 

oc 

CM 

t^ 

% 

v~ 

M 

c 

J 

o  0000  o  00000. 

bi  60      60      to      bo  bo  bobJBbobobo^ 

a       .g  .a  .s  .a  .s  «  5  .a.a  .a  .a  § 

ffi                 h  h       h       h       h  hi  h    t-s'l-J    h    h    W 


■J              N              N                        N 

;     !     ;     1       '.       '.'.'.'.'.&         n' 

N 

N 

H 

ba 

i 

C3 

s 

i 

-! 

hJ 

hJ 

hJ 

0000 

2    2    3    3 
0000 


o    o  o    o    o   -g 

3  22  3  2" 

O   OO   O   O   hJ 


?5   is! 


S5  % 


298 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  2: 


alOJjBq — ^otipcud  ibiiui 


190J— md8p\B}OX, 


•^99j— mdap  no 


t^  CO 

CO  <o     '  CO  >o 


o»ao  oo 

00ttl«©N 
03  0>(D(0  0) 


CO  lO 


lOOO 


££ 


Rcocfi 


►a 

o 

u 

I 

co 

o 


ran^p  GAoq'B  gpn^iqiy 


r~  oo  ■*  i •-  co  i^- 


•OONOHM     00 


ONTflNNVOiOOOWWOOOltCtO' 


188J— I9A81 

B8S   .Avopq    epnjpjy 


•^98J— 

pg^Jigtrgd  ssausioiqj, 


•}99;— do^  o^  q^dga; 


3  o  ej  c3  p)  o 


ft  • 

03  C 

2£ 


13  o 
02 


'IMffiN00nHf[^lOcr.tOHiO<OMtOr- 


CO  -*l  CO  •*<  CO  ' 


;8£  : 


WtOMNlOHOlOl'-XOO 


OfOJOl 


OOOiONiOOiOCCOtCnO«30flONiO( 
(DOCNHINNHHWnlNM^HOtl'Hffli 


ONOJN     CO 


ft£ 


WW 


.a  o  s 

MSw 


-3  *- 

OO 
O  ft 
!>  ©£ 


-3  o 
W    '• 


-a  ■ 

o  • 

o  • 

fc  : 

*  o 


r^  CO  WIN 

cJoJo  o° 
S3  pi  o  o  ft 

•j^'O'd  ps  ps.s.S*fi 
co    I   .'cspq^WW 


o  o  o 

ftftft 

<S>  <D  <D 

W)  ox  or; 

if'd'doco    o 

*n  'CG  ^  ^  "O  3 

pqcGpQ  :  :  :  w 


o 

o 

o  o  3  o  © 

fc 

fc 

BfcgBfc 

3 

a 

rns 
rns 

ler, 

3 

3 

ca 

CC 

pqpPEntsj 

c  o    ^ 


o  a 


o  o 

-*      lO!OH«CO 
CO      CO  CO 


33  3 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


299 


^H 


55'- 

00  "^ 

sot 

>     „o) 


■■afi 

•at 

-  CSg 


05   05 

a  a 
o  o 
-d-d 

fl  B 


££ 


G^1 
OOJi 

■d    - 


££ 


KT>>c2 

5=1  ~   5=1  '• 

h3      h3 


ftp) 


CM  CO  "Si  »0 


lO  co      o 


-ON 

oa  t  o 

ooo 


iOO< 

S3! 


co  ia  oc  io  co  o  >c    CO    t>  ( 

lOXrtiOf  OCR     »C     CT>  ' 

—    o< 


O  CO  >-i  O  O  CO -<r 


'OOOOCOt^CO         CN         ICN( 
(NOCOICN         CO         NM 

©Tt<< 


COOOOOUDGV 


MONlCT)iO«5  t~-  COO 
vhoOtjiiohO  Tfi  O  CO 
•<*  00  CO  ■*  rfi  00  O     -^     •*  Tji 


t~MtCONMN*5TC  00  U5M 
lOWWNWHVN  CO  I--  CM 
t  ■>*<  T»l  Tfrl  Tjl  kO  00  **■  o        t-h         "W  o 


wwho 


i  CN  \rs     in    io 


iO  m  o       T  CM 


8  $  ass 


TH  CO 


aooo    o>    coo      hio 

litr-H-fl       *C       Tfli-105  i-lO) 

00  O  OJ     CN     Tt<  *o  lO       COCO 


NOOWdWO     CO     ON 
OS  CO  CO  C5  Ci  IO  lO     Oi     IOO 
"     00O) 


00  <N  00  00  00  <N  ■ 


io  io      O)05d05  0i0( 


'  oo  co  CN 
>  tji  CT>  iO 


T3  O  O 

cq  :  : 


"d     -"d  W 
O    •  o      co 


03  o 


OcJOO 
05   o3  05   05 

•dtJ-d-d  CE-g    -d 


o  o 

PhPh 
05   05 

b£  bjO 

CCfC 


o  c 

05   05 

t/.  be 

•cd  o 

fcpa  : 


•d-d 
o  o 
o  o 

££ 

(35 


cm    • 

CO 

co    ! 

k 

c 

■  H  fd 
.  03  O  o 

•d 

e 

<  •  p  fto 

o 

P<o  P-iO 

6 

•  :? 

b£t> 

IS 

So  R 

&f* 

'doc 

•CC0 

pq  :  : 


Cd  o 

:w  : 


pcWfcW 


U50COH 

IO  CO  IO  CO 


3     be 

•o3  5 

si  a 


bo        bi) 
bo  bO 

C5        O 


o 
"1   £ 

to    •^  O 
bC 

hi 


-i-T  ^ 
d 


cn  6  6 


o 


J>.       -,  ^    ^  ^ 


w<i  go3§ 


OOhO 

n   n   r-    rt 

S  S  §  S 

OSp,3 
fOpScOfQ 


o      o 


II 

o  o 


B  B 

c  o  o  o 

SB  B.Bf.2f 


2  8; 


3  SSS 
0000 

.5f.2f.Bf.xP  § 

S'pp'bS  pi 

co  r^  00  c35  o 

CNCN  <NCN  CO 


03         03 

h3      J 


300 


OIL  FIELDS  OF  CEAWFOKD  AND  LAWKENCE  COUNTIES,     [bull.  no.  22 


tf^z 


o  o 


ipjJBq— ;onpoad  p3i;iui 


•}99j— itfdgp  \v%o  j. 


•leaj— qidgp  no 


CM  O.  C 


CO 

o 
Eh 

so 

o 

Si 

t 

1 

o 

o 
8 
to 

i 

e 


|  ^99J— 9ire]d 

tnrn'Bp  aAoqe  apn^i^V 


OS  "O  >0  CT5  rr  O  Oi 


199J— I9A0I 

■B9S    j&opq    gpn^i^V 


•"f  O^iOOi 


•199J— 
p9^Ji9U9d  ssgu^orqjj 


.-i  10 ->=»  r^  co  < 


•^99J— dO}  0)  Xl^d9Q 


01"000«3W( 


go 


O  O  o 

(D  <D  fe- 
MbJ0p» 


'C  -H  'C  'E  >3 

ppWfCttW 


££ 


«o>om 


Tf  1— I  O  iC 
rfi  CD  CO  CD 


-3  C 

"CO 

pq   : 


<  o  o 
i  o  o 

:££ 


S§  :S 


flfl' 


■  Oi  CO  lO  CN 


"<*i-*CNCO< 


00  00  C3  00  00 


•d  o 
•C-O' 


03  C7>  05  C7i  c^ 


OtOMOl 
00  00  00  00< 


co  ic  >— 1 1^- 1~- 1--  io 


'IOCocomcco 


iiOOOCN 
)  00  OS  OS  IO 


T)  o  o  o  o 

m  :  :  :  : 


02 .2  ®  ^.2.2 


co  ■*      ;cn 
6    6     '.6 


i— locrr;     tl;       ,  rr;  Tf  i— i  rH  r-i  co 


©i  ^H 


o  o  of 


oooooooo 


>»  >>>>>.  s>>  >>  S>>  w. 


.    .    .  03    C3    o  c3 eao'Oooooo    o 


tooootMCM    ec 
6  6  6  6  6    6 


02 


^^  L/J  u^  *J^  r~ 1     p**     ^^  p*.  y^  Lfj  uj  t^/  vyj  tyj  l/^  l/j  r— <  r~  +—  w  w  >^  • 

~lO  i-H  CN  CO  "W      O     COl^OOCnOrHNCO^lOCONXOlO^MCO      "J" 

CO  rtrtrlrtHrti-li-lHHNNNN     CN 


BLATCHLEY] 


TABLES   OF    WELL   DATA. 


301 


2fe 


oo  a 


g 


§£§§£«§ 


ggSS 


oo    -o 

CNCO     "c5 


g§ 


8  :  :S 


<*«  »«  t^  f~  (M  <N  ©  to 

HOMNONOM 
O)  ©  ©  ©  ©  ©  ©  © 


32£  :S3 

>o  ioeo    •  »oco 


OlOMNINOOTCtO 

St~-  t— O  t^  i-H  00  CO 
oo  oo  oo  oo  os  oo  © 


NCOOlO 
OCN  CO  CO 

to  »o  io  »o 


CO      .  00  »0      •  lO 
tt  lO      •'  CO  lO      •  CO 


i  rococo    .to 

.©O0CN      •!>• 
■  00-«*iO     -CM 


§g! 


r>-  r^co  ©< 

OOOO! 


lOOONN-HtOlONOO'* 
>OCN<0<Or-.t^t^-Si<NCN 

iw^o^wwcoto'v 


'WTticoOiOTrcOi-iLO'OiiiiO' 


T)1TjlTj<Tj<TCO-,»|-"3<< 


>  ^  ^3"  O  "*t<  O  ^  O  ' 


'OtOOf  00!DI"*!0 


^  TJ.  "W  "tfi  T)1  TJ<  •*  *<J<  TH  ,-H  »-l  O  O  "*  O  rH  ,-H  ,-H  00  © 


iNW^OONTj-^moONMNtrtHTPCOcOOOOOOOHT 
iOOOOWOOBOOOO^OV 


,     CN  lOCOCS  ©CN  w 
>rt<000000000^'^,00^-000 


°.  :    Scn£<c 


noowoo 
.-icn.-icocn 


ICMr-ICNCN 


I IM  i-<  CN  T*  CO  CN  CN  i-H      ItOCSCN     •     'OOtO 


IHN00NNMK5O! 


looioom-HtoNtoo'w 

iNLONXOOMt'OHH 
>lOlOiO00-<fiO»OCOCOiO 


MfflOliONMCO'tf  Ol 
OOt^HBOHWO! 
T}iiO'^lO'*iCO'0>OCO( 


l'»<rJ<00iOO5iO00'VOCOCNOJTliO500CNCN'>»i( 


*o  o  o 

pq  :  : 


.  o    .  o    .  o  o 
.  g,  .  a  .  q,p. 

.CD     .CD     .  CD  CO 

.  be   .  oo   .  bobx) 

co  o-o  ceo 
X5  -e  "O  "E  "O  *E  '£ 

:pq  :pa  :po« 


o 
o 

% 

•a -co 
M  :  : 


>-o£ 
?E-ar 


OflO 

.£££ 

-o-a  cj.s 

:MpqM 


•-hcn  ;  !,7iC?   ! 

•"'O'O'O  a-o'o  a 

•  OOOOJOOtJ 

o  o  o  a  o  o  a 

1  ■  >a  ■  ■ 


n  CN 


•CN    .cn 

-    ■  S<o  £<o  P<o  o  a    •   •  o 

>2£5£:2,2,*S,§00£ 


•o-o.a.a.a  a -a  .a  S'o.a'OE-a'E-a-E-a.a  p-O'O.a 


-o  eg 


■o.a  § 


tt  cn  io  r»  oo  to  to  co    t^ 


•  cn    cn    eNt^eo    oo 
I  oo    io    to  ■>«•  >o    CO 


ICO      i-H      -Jli 
i  lO     T     ■<*<  i 


ICO     ©     00     lO     OOCN     CN     CNi-H^     .-H     o 
i  tJ«     rr     t}<     rji     -rfiTi     lO     »OlO»0     »0     lO 


•O     •©©©     'hi  "tf 

i-l  CO  »0  -iCN  CO  CO  55  9 

^  M 

O  O  ©  O  O  o  o*e  m 

55  55  55  55  55  55  55  <?  § 

.......     .s     ..      „•"" '  H 

CDCDCDCDCDCDCDtq  P 

OOOOOOO+a  rQ 

-      -    n   r-t  H-l 


HNMO      O 

55   55 


o 

'££  2 

o  o  o  ^  ^  6  ,^55  £5 

ZZ 55.2*  .oo   55  cd  ^  aT 

a"  a"  a"  |  |  a"~m  2  'i 

rf  ^  &     •     ^j      C3     .i-^  • 


co<n 
6  6 


a"  a"  a   a* 


15    w    O    h 


o    d  d  o'    d    d 


o    o    o    o     OCN 

.§.§  5  ^  a"  fl   a"  a"  a  a^S  "3  "3  "3  [3  a"  a  a"  a"  a"  a"  a" 

(^ii^ii^^O      O      O      O      OOh     R    R    R    RO      O  OOO  O  O 

uJuJ    i_J    ^J-a    AAA    AA A    A  AAA  A  A 

SS   S   Sb    H    H   H   HEhPh   Ph   Ph   Ph    Ph Eh   Eh  EhEhEh  H  Eh 


oooooooo 

S5S5SS23  a 
oooooooo  o 


OOOO     OOOO     o 

22131a  2  222  2 
OOOO  O  OOO  o 


03  CD      03      CD 

tasa  fa  sa 


;g  A  A  A  A 

"  "  "  "  " 

a  a  a  a  a 

CQ  CQ  CQ  02  02 

^j  =3  ^  <3  =3 


i  ooia  to  w  to  too  o  ooo  o  o 

03   03       CT       03 '3     *3     '3     "3  '3 '3    ™  C3  03  03  03  *3  *3  *3  "3  *2  '3  'Z3 

^5^5    ^3    ^3-a    ^3    ^3    ^3  ^^,3  fl  ^3  .a  AA  •&  AAA  A  A 

coos   02  02O   OOO  OOcc  02  02  02  02O  O  OOO  O  O 


8  8  CN  8  8  8  £8     S§ 


lO     <Ot~00     i-H  rlCN     CO     'S'lO     tO     t-     00     QOh     N     M     f     iO  to     t^     00  < 


02     |55 


302 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.      [bull.  no.  22 


•felGjjBq— }onpojd  \vx\ui 


■laaj— Hldop  i^oj, 


•^aj— iHdsp  no 


o 
» 

1 

S3 

© 

g 

s 
e 


•jaaj— aireid 
rarq'ep  aAoqB  spn^piy 


■B8S    Avopq    apn^t^iv 


pa^jpuad  ssampiq/L 


188.1— do)  oi  t^doo; 


So 


"3  o 


(MOOcCO 


ioooo 

iOOOiO 
ICN<N<M<N 


'O  N  lO  O)  CN  C-l  : 


NVON/OO 
lO  CN  lO  CN  CN  CN  CN 


.  c3 

:£ 

:*a 

t 

;CQ 

8  :* 

band 

475fe 
feet. 

£  :o 

88  :8 

CNCN      -CN 


■00  OiO  CT>  ^  CN  CO 
-.-l-^rt^COCNCOCN  — 


8    £28! 


iNNHOtDHffllO 

I  rt  ■*  O  M  ffl  TP  CO  CO 

ONNNTfNVCOO^l 


NHNOIO. 
(OHHOffiv    _ 


iO>00Nt> 


NO00  TP  00  O 


!  i-(  CN  .-I  i-<  O  < 


NiOOU5!C«MiOO' 


i  T  O  N 


Oiooramoooooioio 
oo^j,coio<Nt»-*anocN'0 

00(NCN(NiOC<|iO<NO)m>0 


gsgs 


>  o  o^ 

:  :  :w 


m  :  : 


T5  PI     .'TlfiSfi 
O  C3     •  O  03  O  c3 


O  C3  O  03  O  c3  O 

iS|i|S| 


1  OS  Oi  CO  CO   CO  CO  CO 
i  CO  co  t^  t-  t-  t—  l^ 


o  >o  o 

CO   CO   l^ 


O  rH  ©  M  O  rt       CO 
t»(NH00      CO      i-l  CO  r-H  i-l  i-l  r-i      CO      CN      CO      i-l  •»*      CO 

dodo    d    dddddd    d    d    d    do    d 


CO        CO     ffl 


o    o    o      o    o 
fc   £   55     55   fc 


2222  S  222222  2  2  2  22  2 

oooo  5  oooooo  5  o  o  55  5 
,3  xs  JS  .3  A  &A&AAJ1  xS  &  ^q  ^3^  £ 
EhEhEhEh   H   HHEHrHeH   H   e   B   eB  ch 


,3   X5   A 
H   H   Eh 


X5   .a 
Eh   Eh 


oooo    o    oooooo    o    o    o    o  o    o 

3333  3  333333  13  32  33  3 
oooo  o  oooooo  o  o  o  oo  o 


o    o 

3  3  3 
o  o  o 


o    o      o 

3  3    3 

o  o    o 


S3  SSI 


IB 


O     <-i     CN        CO     •f        uO 


.ATCHLET] 


TABLES    OF    WELL   DATA. 


303 


:§§S 

NHrH 


CO  CO  CM  CO 


00  COO 

f    T-H    Tj< 

lO  CO  CO 


SS8 

00  CO  CO 


&«d 


pl-O 
C0£ 


wo 

CO  lO 


©loow  ira 


o>o 

lOCO 


MMSHisooawa  cv 


OOOWOOiOiO^OO^i 
OI-MOHHOONM 
■^iTjirf'ai-TiO-^lCO-^CO 


f-—icocM-*cooai. 


IHWMCO 


l~  :o  n  l~  :?  r- 


TfO^NOOOMOOWO 


O  O  O  O  O  00  c 


OOOOOOHOOfflO. 


I  co  oo  r^  i>oo 


NMHHHt 


<M  <N  CO  CO 


>  OS  Tji  CO  CM  < 


CM  CO  (M  lO  Tf  ^H 
i-H  t^  CM  i-i  CO  CM 


•  COCO      "-ICOCOCO 


■0593°° 


CO  (M  CM  CM  -^i  1 


>  cm  *o  -N  co  0  to : 


ooNMooaoMooooom 


3-0 

»  : 


^HCM 

o  o 
o  o 

0  0444* 

7373.3.=; 

:  :^Ld 


2  c 

—  o 

-  > 

-I-  -- 


-r  0 
o  - 

4^-r 


)73  d73 
)  O  C3  O 

>pflp 
:fcjc3£ 


£  : 

£   0 

.-  — 
M   : 


•  t3  t3  d  t3  t3  t3  t3 

•  O  O  03  O  O  O  O 

•  o  o  pi  o  o  o  o 
O  44  4*i  -g  44  M  44  44 


fl73 
c3  O 

d  9 

Cj    £ 


73  d 

O  c3 

oa 


1-lCM 

^73  73  -Id 
=  ,>>  £  o  £     . 

■3  5^^5-3  o 


■MMffl  M 


3—1 73  3 73 .-1  di3,<-*',~<  f  ^ 


r^  00    e»    03  00    o>    co  co  x  < 

Tf>  f       lO       OlO       lO       lO»OTf<' 


s  s 


N     OS1     O 


S  <*"  8 


.iOOOh     N  tJi 

r-{  t~-  CM  t-h  CM  CM  CO     CO  CO 

0    6  6  6    6    6  6    6    6606666    6       6 


0000000 

£  £  fc  ££  £  £ 


CO  f  t~-00 


©       CE>   CD   CD       ©       CD   CD       CD       CD   ©    ^    ©   <D   ®    $       CD 

0,0,52  d  dd  d  g  "3  g  "3  g g g dgS d  d 
sirirl  S  www  5  ww  w  wwwwwww  w 
SSSS  h  www  w  ww  w  wwwwwww  w 


q)      (D      CD      (p   CD      $      CD 

[3  [3  q  d  d  d  d 
W  W  W  WW  w  w 
w  W  W  WW  w  w 

£££££££ 


CO 

id 

Of      H       H! 


00     O     OO     o 


OOflOQfl 


2  2  2  2 
3I3S2 
->ooo 


®      ®  CS  CD 

•d    ^^3^5 

CD       CC    CD 

^3    ^5X5 

i 

rt 

CD  CD  CD   CD  CD   CD  CD 

CD 

^3 

,d 

CD 

5 

CD   CD 

J3  J 

CD 

42 

CD 

xi 

3 
4: 

C3      03  C3  c3 

C3     c3  c3 

Ifl 

01 

03 

rrl 

rfl 

CI 

c3  o3 

on 

rfl 

3   333 

3   S3 

3 

3333333 

5 

3 

3 

3 

3 

S3 

3 

3 

3 

02    CQCQ02 

CQ    CCCQ 

CO 

CO  CO  CO  CO  CO  CO  CO 

co 

CO 

DD 

CO 

CO 

coco 

CO 

to 

CO 

^5  =3°<J=<J 

^}  "3°3 

4 

c^^^^ 

•8 

<« 

-3 

<8 

<J 

=3^5 

•8 

<« 

•8 

ki       Uhh 

t-i 

C3     C3  c3  c3 

^  ^^g 

§ 

6|||»fu 

C3 

c3 

SB 

tl 

99 

c3  a 

a 

n 

fl 

XJ    ^^^5 

^2.    ^3^! 

^3 

,q  ,q  ,3  .d  ,d  ,d  .d 

*J 

^3 

ja 

^5 

X 

-dxj 

43 

4= 

4= 

CO     C0CQC0 

CO    COCO 

OQ 

CO  CO  CO  CO  CO  CO  CO 

ta 

CO 

Q§ 

CO 

CO 

coco 

CO 

X' 

QQ 

CMco-<r    uo 


00  OS  O  rt  CM  CO  f  lO     CO 


2  8 


000 

d  32  3 


00  o  00  o 


304 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


•siaueq— jonpoad  ibi^toi 


SoiooioNpimo! 
t-icoi-i^(Mcncncncn< 


•^a;— tfldap  pno  j, 


mono 

lOCOCO 


5DNCO>OteMC01'lONO>ON«00> 
O"OtONiO0000!0O00O00t0U5T)i|N 

t^cococococococo'fco'tf'cococococo 


•199j— mdep  no 


IO  CO  CO  CO  CO 


§ 

© 

o 
to 


ran^p  8Aoq«  apnimv 


CNCOTtH^^HOiCOCOl 


SV5DmrtHO>OC005C0ONONNN00(»TI'O 
lO'OCOCO-fCO'*t<lOlO-'»<COCO"t<lOCN''»'iOt^OOt"- 
t—^COCOcOCOCOCOCOCOCOCOCOCDCOCOCOCOCOCOCO 


■Gas   .Aiojaq   epn^jy 


ooooooooooooooo 


OtO^NOJOlOiONHNOPSOKlCSOONNtOO 

OTt<Tt<cocoiO's,iOTti'!j<iOTticoto->rr^iO'<j,c^i— i  co 
oooqoooooi-iooooooooqooooooooooooooooocooc 


ooioioomiNicoTfoooooioo    .00 

OOMNCOOHN        (NNHNNN      •        ^-t 


•  Tf  tototoo 


•}aaj— doj  01  mdea: 


■*01'OOOOONNH!Oi0  10  01lOOOOOMON 
COlOCOCOCOCOCOCOCOCOCOCOCOCOCO-9<COCOCOCOCO 


pq   : 


gsgsgs 


DC 

£9 


£73 

•-  z 

I* 


'"O  •£*     3   'O  ^  'O  ^   *0   '"O   ""O  ""O  'O   "^   ^  ^ 

:Mm  :::::::::::: 


cq«2  «  >.2.£ 


IO         <N      CO-* 


*     OM 
to     00  00 


I  TJ1       T}i       •*»<  IO  »C  T*1  kO  *0  I 


lO  iO  10  to  ifl  iO  1 


00     O     OOOO 


X 


iO  t^©T»< 


'hoo    >-i      t~      »-h    10  cn    i-h     si  e    a>    <x>  ©  cc  ©  <o  co  cn  ■ 

0000      o      o    00    o    flfl    fl   .9.S.S.S  6  6  6  0  6  6  £  £  £  Z  Z 

fe  &  fe    <3      &      fe    fefe    fe  HW   H   WHWH m&MMMM  cd  ®  &  ®  ® 


1 

C3  O 

3?!5 


g . 

•rt  o 

8* 

CO 


cc      to  to  co  co 


000 


a>  cp    cp    cd  cp  cp  cp 

56  6  6666 

03  c3     03     d  ci  ci  c3 

aa  a  aaaa 

OOCQ    CO    CQCQCOCG 

L-    •_        fc-        (_    In     t_     S-i 
CP   CP       CP       CP   CP   CD   CD 

o      o    00    o  WW  W  fctatafgooooooooooo 

323  3    3   2  23  3  ^2  ^  ,§12,533333333^^^ 

OOP   OOP   OO   O   cqcq   ro   cqcqcqcqOOOOOOOOOOO 

CMCO-*     >0        CO        I>     OOOi     O     <-HCN     CO     ViCtONOOO>OH(NC<5-*iC(ONCO 
CO  CO  CO     CO        CO        CO     COCO     t»i  rtrtHHHHHrtH 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


305 


o  mo  o  ( 

NNrHNi 


oooo  < 

lO  O  IO  o  < 
NINON. 


«o  O  05 

CD  t>  - 


»o© 

ON 


£j££ 


S|S8 

02 


COOOiONOO 


l~-     .  cq  tji  co  ■ 


©OS 
•"f  i—i 
COCO 


HOOOOONO* 
IONNNH00O! 
CO  CO  CO  CO  CO©  N 


CO  N  O  ©  "O 
OiWHCROO 
N  CO  CONN 


>Tf<NrHt^.cOcOcOCOCOl--CO-<T> 


00  ©   iO  00   CO  N 

t>-  oo   oo  ©   r~  to 

too   COO   to  CO 


i  CO  CO  O  O  N  CO  CO 


00  CO  00  00  CO  »o 

SgoS-^° 


ONJO 


t~-  iO  ■*  CO  CO  N  i 


r^aoNcococc'fN'fOcocoiO'-H 

NNcoNot^omr-K0500^^ 
ooooooooooTri>-oooNcor-oooo 


O  N  -V  t^  1^-  < 


N  rH         IO  N         r^  00 
N  rH        i-(  O        N  tj< 

oo  »o      oo  io      oo  oo 


iiOOOt*-*         INNNCtMOOOOOiN 


S  :S3  :SS8n£ 


INiOCH 


>  io  io  o  co 


HMNNi 


©©iO>OCONNN0000 


■OSNNO-^OOCO'T  C 


■COOIOOOONr^OOOi 


ICOiOt^OONCONCOCOl 


N  "O  OS  tO  ©  -9< 
CO  N  N  .-H  rr  iO 
CO  O        CO  O        COCO 


©©OOiO-*  iON 
©NCO©CON00© 


OiOOO"O«00tDM 
lOGSlOOCNOCOt-iai 

OOHN^iflOtONi 


I:  a 

O  c3 


r-<N        • 

a  a  pi 


P-S  b_5Sr^-cj<?l 


c 
o 


ooooo'd'ocs-HSoooo00©00' 
•d-dxJ'd'd-c  sis-S  2  o  3  S  d'd'tf -d-d-a.^ 
:  :  :  :  :cqparaWe-iSPQpqpa  :  :  :  :  :M 


PI  C 

03  O 

PI  9< 


-s-a 

pq  PO- 


ST; 

mm 


Nep 

cJOcJ.O.  ...03.OOO-, 


NHOO'* 
CM  OS  OS  O0  O 
iCJ  "&  ^  ■*!  iO 


t—      t^  00  O  CO  CO 


S3  S 


i-l  i-(  rH  OS  t- 

6  6  6  6  6 

£££££ 

gg"  see' 

cd  co  53  CD  o 
bfi  bfi  bfi  ta  M 
O  O  O  O  O 
PhPhPmPhPm 


CO     iO  CO  ■"*  N  i-H     i-h      CD 

6    06666    6    S 


CD      CD  CD  CD  CD  CD      CD 

bfi    bo  be  M)  bfi  bfi    to 

O      OOOOO     o 

tf  pntfpstfpH  pi 


0 

0 

0 

0 

0    0 

fc 

to 

fe 

fe 

£ 

to  to 

"3 

"© 

a 

pi 

pi 

pi 

a    pi 

pi 

pi 

a 

el 

a 

a    Pl 

0 

0 

0 

0 

0 

0   0 

P 

A 

P 

P 

P 

P  P 

O 

O 

0 

O 

O 

O  O 

OOOOO 

33  32313 

OOOOO 


o    00000    d    >> 

3  32333  2  £ 

O  OOOOO  o  o 


pq    m 


PQ  PQ 

PI  PI 

CD  CD 

-a  -d 

o  o 

P!  PI 

02  02 


I©  H  N  CO 

INNN  N 


f    ~    ~      -h     h 


t-»    00 


—20  G 


30G 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


•spxTBq— lonpojd  XBjini 


•;aoj— ttfdap  i^o  & 


•}09;— q;d8p  po 


.2 

o 
O 

! 


tnni'Bp  aAoq-e  apn^niV 


•189J— I8A8I 

■B8S    MOiaq   epnjT^xy 


parej^aued  ssau^oiqj, 


•}98j— do^  o^  mdea: 


to  .  ,  Li 

3  O  O   C3   fi  0 
CO  <2  «  >  .2  £ 


o  « 

02  O 


**** 


co    .cocococo 


S8 


OMOM  Tj^COiOLOOO^OcOiO^rt^cO^CJiC^CDCO^COC©!-''-^'??' 


■*lOO)0)rHN( 


r-H->*l-<J<CJiI^Tiai<3}(N 


CN'*-!l<U:00OOOHN*t0N^M»00'<tH00'<*U500OHHlMN( 


o    . 

33  o 

8* 


nooHooNoo©NNioK50oowoon 


t,  a 

O  03 

ftfl 
,d 


d-dd-d-d  d  b 

c3  O  O  O  O  C3  O 

pooooflft 


"C  dZ; 

O  03  O 

ft  d  ft 


sSsssSas^s^a^ssssi 


•d 

•fl  d 

PQPQ 


it3rdld    .    . 

!  O  O  Ort(N 
I  O  O  O    '     J 


l-dd  3 


Ch  d'd' 


l-dd- 


«  :  :pa3Qi2i2«maapami»pa  :wmw  :pq33S££co 


fc    £ 


pp 

PQ 

pq 

PQ 

pq 

PQ 

PC 

w 

Pi 

d 

d 

d 

c 

d 

d 

d 

<D 

•s 

d 

d 

•d 

d 

►d 

«d 

•d 

i 

£ 

fe 

£ 

£ 

£ 

£ 

is 

o 

o 

o 

o 

o 

o 

a 

d 

d 

d 

d 

d 

fl 

a 

CO 

CO 

CO 

CO 

CO 

CO 

CO 

CO 

CO 

IO 

CD 

t^ 

H 

Ice 

BLATCHLEY] 


TABLES    OF    WELL   DATA. 


307 


O  CO 

;o 

C3  03 

!  =3 

££ 

•S* 

•*J  -1-3 

cS  T5 

J1TS1 

.co 

03  ~ 


££ 


iO  tji  cd  iC  lo 


(-  o  o 


o    ~B,cd,cd 

~  S-i    C3  ^ 

-■^  %»  co  O 

P*"  C3  03 


i  a  ►■a 

'O        CO 


oi  o  ■»  r-  o  w 
coco  coco  coco 


ooo 

CD  CO  O 

f-Tt-TlH        CN         1-lrH 


.    _   O         tO         !>■  CO 
<N  <N  ■*        i-H        O  CN 

CO  CO  CO        O        lOffl 


OOiOO 


iO  iO 
I~-  00 

CO  CO 


or^oeN 

MiOiOiO 


s.   ~ 


)0)00NOffl*KIO0)»t01'ffl!OfflOOOt0O 


rH  -HCO 

oo  r-  t- 

COCCCO 


COCO        00lO( 


NNINNLOOiNNrHMMNMtCHtONOl' 

o^<-HC5C^r^^T±irtCN^eNr>cocococNCN' 


ooiofflooo»ooooooooi<ooio 


NNO)Cni»cCrtO)Oi 
OOOOOOlOOOOOrtOOi 


IcSgS? 


OOONHOVWOOiOfflNfOHHO 
>-l  C5  CO  CN  "*  iO  00  CO  i-h  O  CN  t-  CO        <N«MH 


onoooNociiflo 

1-lCNCNt^.i-HCOiOCOiO 


1  OCR  O  O  <N  O 


lOtOOHtOOiOiOO) 

lO0CT>O0QOH00HMH(DCOCO'*i-IHTl<Ht^         (NLOt^cOtMCOtDN(D 

>  CM  00  CN  Tf  CO  <M  O  i-i  CO  iO  CO  CO  CO  CO  CO  Gi  CO  O 


ONOCDOO' 
I  LO  t^  CO  "*  CO  I  _    _ 

co  «  co  o  co  m  m  io  «  io 


ICIO  i-H' 


O  CSO 
O  Pi  Ph 

£28, 


■doo 

pa  :  : 


■s^-sfi-g-s^o-g 


J  O  C3 

s  o  a 
iWcq  : 


O  c3  o 
ftfl  O 


C3  O 
PS  o 


B 

e|l  - 

ipqpqpq     pq    :   :pqpqW   :   :pQM 


o     •     • 
o     •     • 

*  :  : 

£  o  o 

.£!  "B  'B      'd 

M  :  :     : 


O  c3     •   O 

ftc  :  o 

TJ  d  o3  .S^ 

pqpqO^co 


>OH35 

i  iC5«C-* 


r-HClOO     00 


0OCO     — i     CNCOO     iO     NWCOCDCDS 

O  O      O      CO  lO  CO      »C      MOlOCLOI- 
mm     O     Ttirfrji     th     --fiTtiTr'-<jiTt<-*i 


n 

CO 

CO 

•oim'toHH 

y-t 

<N 

o 

o 

o 

o  o  c  o  o 

o 

O 

*A 

fc 

fe 

£££££ 

£ 

55 

; — 

_r 

_^ 

r-TrTr-T.  Ti-T 

p 

r 

CD   CD    CD   CD    <D 

M 

R 

a 

fl    PI   fl    3    fl 

d 

d 

p 

a 

a 

B 

d 

o 

o  o  o  o  o 

o 

o 

Q 

p 

0 

CQfiQQ 

P 

A 

O 

o 

o 

ooooo 

O 

O 

~3      CO       OOO       O 

»     a>*   cn   £££   £   ^eieo'eow 

ii  i  in  |  niiii 
fi  I  lis s  iiflll 

p!  p|  p|  .  .  .  .  P  m  R  •— «  .-h  .— . 
OO  O  rvi  M  rvi  M  «5  o3  eS  jr  J^  j£ 
qp p      ...      . OQOOOO 

bb  b  ^b^^'  ^  PH*p-!p-l-<<i<i 


2?   £ 


o  o 


pq       pq       pqpqpqpqpo  pq 
d    d 


d  d  d  d 

CD   CD  CD  CD 
'O  'B  'B  'B 

££££ 
o  o  o  o 

d  a  pi  d 

CO  CO  CO  CO 


-b  >d 


«2  £  £  £ 

CD  CD   CD  CD 

555  5 

h   2   S££  S 

pqpq  pq  cococo  co 

d  d    d  ^j^^  ^5 

CD  CD      CD      i,Z.i,  Z. 

££    ^  cg?g?2  g 

O  O      O      CC?  c3  C3  c3 

d  d    d  ^i^x! 


d  d-d 

fell 

ooo 

C  fl  d      - 

G^^  ooo      o      o  o 

H  9p  b  23  332    23    2323 

coco   co   cococo   co   D^DOOO     O     OO 


CM  CN  CN  CN  CM 


308 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


•siozreq— jonpcud  ibiitui 


•^99j— itfdop  pno  j, 


•laaj—mdap  \\q 


a> 

d 

o 
O 

i 

CO 

g 

o 

§• 

«1 


•^9o; — atrejd 
tanjBp  aAoq'B  apnipiv 


B8S    Avopq    apri-ji^y 


pe^j^irad  ssaujpiqj, 


•}88j— do;  o;  q^daa 


w-2«  >.2. 


c?o 


0Q 


88 


2§ 

C3.Q 
73  t> 


cQSSS 


OO 
88 


r-  co  c  ■-  cc  c=  * 
iO  ©  OC  OO  00  « to 
CO  CO  CO  COCO  coco 


r-     ■  t^-  *  1-h  a> 
*     ■Noooor- 

CO      •  CO  CO  CO  CO 


OtOtOOO*r^oO*OOcOto 


oi  *  a>  o  co  <N  • 


MtOtOtOtOI 


_    .liHiOCONCOt 

coiotONOr-totoco^toi 

COCOCOCOCNcOcOCOCOCOCOt 


coooooo 

10*10* 
tOfflH* 


00C5  O  CT>  COO  O  *  00C-      - 
OOOi-HCNOOr-IOOOOOOOOCN 


HtOHC*0OO!lON00N*t*tO 

co*cococb<Ncococoioco*cot-~ 
ooooooascstccooooooocoooooooo 


HOW        OiO 


88; 


NtO      'NiOON        ONiOtOOOIN'0(N(N*tO^ 


2ci: 


88S2 
i-H  *  CO  OS 


--H*CNCOOCOr-llO*t-ICNOOCO' 


O  CO  CO  l^  CO  f»  CO  CO  CO  ■ 


pqcccoM 


£  2^    '  S^  s 

O  c3  O         C3  O  C3 


oooh    co    ""^S 

to  to  to     to     to  to  tO 


088 

to  to  to 


38S8 
to  to  to  to 


<M  CO  *  i-l      •      ■      • » 

i-li-lrH^H*COCMe5 


o  o  o    o 


ooo    o    oooooooooo 


xJ      0>  G?  C2      ©  05  02  ' 


o  o    ooo    o        ooo    o    oooooooooo 

a     a  a a a  a    aaa  a  aaaaaaaaaa 

O  O    OOO    O        OOO    O    OOOOOOOOOO 


ON     CO*  to     CO 


t^OOOJ     O     ^H  .-H  CN  CO  *  lO  CO  t>  00  i 


w 

w 

CO 

8 

£ 

BLATCHLEY] 


TABLES    OF    WELL   DATA. 


309 


"^3  c3'S  OS 


OS* 


1 02     ■     .02Pn       02 


©  © 
tart 


02« 


03  d  OX) 


o  o 
.d-d 

02  02 


oo 

ofc<r 


SCOOOOKOOtOO 
moooooo 

0«0^        0)«OCCH 


OtOirtrtHlOtOiflO         f-  ^  CO  O  CD  i— l  CO  "fl         ffi*ffi"CiOWOO         OOlOO 
NiONNNOJHlPO         i-Hi-ITfiOi'-fCOCNTfl         lO  i-HO  (M  Ol  <£>  N  (D         OOVO 

H(NHioTt«cqHiNiN      hhhoooio^      HHHMeioeoN      i-ii-ti-i 


IOOSO>W*CO 


ootOTji^TriCi-^to      *!DHir,ioiooo      phoh 

00  O0  lO  O  lO  tO  t~-  lO    •>*  O0  "*i  t—  O  CO  00  tf    i-H  lO  Oi 

COMM^ItlOOJO         00  CO  CO  tO  00  O  i-H  <M         00  CO  CO 


OOOIMOOOCO 

HHMNlOlOMH 


•^iT-iOOOOOiO 


o  o  o  o  io      owaimoNoo      tooi 

VNCOTH  HHNONOOMN       <N<M. 


OU0TKOOO! 
lO  Oi  O  O  O  O  < 
Tfi  lO  OS  rH  TP  t-  < 


•  OHOotoiomo 

NlOrtHOOtOtCO) 

t^oo-t<iot©oot~oo 


>iOOOC"00<N 
>  t£  CO  OO  CO  Tfi  lO  CO 
)  00  00  00  CT>  O  T  lO 


iNHiOiO«3( 


J  o  o 

)  tO  CT>  <M  <N  CO 
I  i-i  <N  tji  to  l> 


'CSS 
PQfflPQ 


M02W«02 


:QkQ 


-H  NtO     N 


000 


s§  s 


0<N 

©  o 
a-  o 

C3 


6  0  o 

0     -    --T 


MM  WW 


000 

S3  2 

OO  c 


,d 
s 

02 

.  © 


©,d ^a  © 
na  oooco 

1^1 


CO  -*1 10  to 


^z 


310 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sjaxreq— ;onpoad  renim 


188j— qjdep  i^ioj, 


'laaj— q^dap  no 


•^j— atrejd 


•}88J— I8A81 

■Bas    Avojaq     aprnx^y 


pa^j^uad  ssau^oiqi, 


•^88j— do;  o;  qidaci 


3  o  a>  c3  a  © 
zo£  a!  ^.242 


X3  O 


►  »?►    - 


££ 


S8 


+J  «o 


C>3  c3 


c3  O'Tj 
OHto 


03  50 


£ 


c 

»-  O 


<Mi^-ogo3i--r^H      o  -en  ^h  os  co 


I  OS  00  -<*i  CO  CO 


as  os      sjogioeocoooocooscocooo      10 

OS  -f         MOOMOOOlNOOXOrHOM        -^f 
OSLO       CN        i-H  OS  O0  CO  >0  tJ<  tj<  CO  ON  1-1 


N  N  N  LO  N  O  t—  CN  ■— I  OS  OS  •— I  i- 1  *N>ONNONNrtTH[^N  10 
NNHOINOI  OS  iO  00  O  CO  OiO  NiHCDCOWOOHHOSXatO  lO 
MHJOOHH        Nc 


OS  -T  CO  i-l  Tf  O         rtCOOSCNOO 
XOHOtON        OOOOOOOSOS 


o  o  oo  o  co     om-^iNN      oo      lOHoooonmo^NOio      oo 

—  LO        t-  H  O  ■*  N  X  -n  M  ^  M  O  O        lO 

-*      t^  os  oo  o  i-i  co -^  to  io  co  oo  oo      os 


^SS  O  O  C3 
•fl  T5  T3  5  3  ^ 

PQ    :    IfQpqra 


•i-HCNCO 

o  o  o 
o  o  o 

.  .£££    , 

oo££.£     -do 


CNCO 

fl  d  a 


fl  fl 


CD 


.-3  «H 

08  £  12.2  .2  c3oo  O   C8  - 


a  a 


o  o 


BL.ATCHLEY] 


TABLES    OF    WELL   DATA. 


311 


=3  a 


g  : 

o     • 

i* 

££ 

«S  co 
05 

S3  w 


lO  O  CN  O 

cc  CN  cd  co 


CO^HOO 

oascom 

O  CO  CO  o 


ilMO^N 


lO   -W   TJ1 


—    /    ?ll-(NOOi 


i  O  h  O  lO  i 


■.MHMHOHHOU 


'NNCNCCI 


iooioowion 

IWOlOCOlOWiO 

imioiooaoo 


CO  ■"»!  CO  CC  CO  iO 


0SOiO>Or^0SOS0S-*0:OS^H-<f000000-*t<C0CN» 


OMtOOiCN         COrtC<IOOCOCCCNOSO- 

OS  CO  i-t  OS  <N         HHHOJt'ONONffiNONMrtHNOM 

XCOiOOOrH   CO  iC  CO  rf  CC  CO  iO  00  00  CN  CC  CO  CO  "9<  CN  co  «o  a> 


CNint^cNCNr>-CNt-iO 

COfOONMieOlOrt' 


cSSS 


m  co  o  o  co 


;2§3£3   ssssssss  iss* 


lOCN  tO< 
I  Tfl  t-  CN  I 


f-OOOOi-HTfiOiO 


NOlOOON 
HINrtCOCOO 

ooooooo© 


CN  f»  iO  rt  it.  -»  00  IO  O  CCNN^OCO  'O  < 
■■  -TCOCNorcNCOCOa>CNOiCOOCO--f<TPOCN< 

looocoooococooocooor  _ 


'OCO^tD      oopooocoocococooococ 


1  OS  !>•  00  i-n  *&  CO  C 


iCNiOiO^iOHOOS 
>l-~OSCOCO00cOCCiO 
IO5MN00CT1OCD 


rHCN 


ft 
as 

6JD 

2,2,2,2,2  03'O'cJ 

pq  :  :  :  Impqpq 


b-s^ 


CN  CO  .-I  CO  i-l  CN 


O  O  O  O  O  O 
ft  ftftft  ft  ft 
CD  CD  CD  CD  CD  CD 
60  60  60  60  60  60 
•d  d  t3  'CJ  13  T3 

pQmpQpqpcm 


OOOo^ 
O  ftftO-^ 


tH     (_     J-,     iH  >C  "E     S-l 

O  O  O  O  o  o  o 
ftftftftO  ftft 


T3  S-hTJ"  s-i   S-.  t-  Si 

o  o  o  o  o  o  o 

O  ftO  ftftftft 

t»  d>   b.  CD  CD   CD  CD 

il>  &o  bo  bobc 


fi-o  j^i-  jh-ci  »-   .  fl-c 

fl  O^  ftftO  ft    •  fl 


MpqcqWS     PQcqmffiMpam^  McQ^PQfQpqpq    IcqM^pqcqWpq    ipoMtrn^. 


«5     "CO     ifl 


lO     lO     lO 


cq 

i> 

CN     iO  CO     t(h 

© 

CO 

i-l     os     CO 

o 

o    o  o    o 

o 

o 

o    o    o 

o 

B 

Sz  ££  £ 

£ 

£ 

£   £  £ 

p 

£h     CN  CN     CN* 

cn" 

CN 

CN     CN     CN 

■J 

+s 

+i     +i^J     +J 

+3 

+» 

-^     +i     +J 

o  o 

CJ   o       _ 


<    <  <  < 


co  co  co 

,Q  ,Q,Q 

B  B8 

o  o  o 


~  ^     ^      £ 


.o    £    £ 

ass 

o    o    o 
O    O    O 


o    o  o    o 

3  32  2 

O  CO  o 


o     o     o      — i      —« 

o  o  o     5    £ 


c 

c 
a: 

[2 

IS 

^ 

H 

&■ 

E£ 

E£ 

E£ 

t 

w 

p£ 

pe 

PS 

P£ 

p£ 

p 

a 

c 
U 

V 

e 
o 

c 
C 

R 

c 

c 
C 

V 

eS 

C 
<<! 

O 

c 
c 

cr 

e 
c 

c 
C 

V 

c 

e 

o 

c 
C 

o 
c 

i-l         CN         CO      -<ti  iC 


312 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sjaxreq— pnpoid  ps^rai 


•laaj— q^dap  pnoj, 


•}88j— q^dap  no 


o 

I 


o 
O 

o 


rarvyep  GAoqis  epn^i^v 


C3    ,0 


NOIH 
lC  CO  CO 

toooo 


•^99  J— I8A8I 

Bas  Avojaq     epn^i^iv 


pa^'Bj'jenad  ssau^oiqj, 


•^98j— do;  o^  q^da<i 


3S32S' 


■i'tigiOMCOOW^'^MOOOOWOO'ftD      CO     lOlOinOOOONlON 
I^t^NOO'J't^MI'OlO^HiONNMOOOlN     t—      f^t^OOrfCit—  OCO0i-im 

<N^no5«ocO'-i'Oi-ioiO5ioeoco(N^HO5a500ioco    i-h    NHOiooiOMHaien 


to<OHOo^*ciHto<owinooo 

NNt-OC0'0(NcDl00)'fl"0   "" 
iMMiOOlHCCOJM'CuOOJH 


H  M  CO  lO  »0  tf)  OJ  iH     CO     NMiO(OO)HCfl>O00l 


O     •     -00     •     -00     •     -OOOCO     •  iO  •*  O  iO  iO  CO  ^     <N        •     >U0     'O 
CO     .     .rti     •     .rH      ■     i-^cOi-H      •  CN  <N  CM  <N  O  CO  i-H     -H        •     •  <N      •  CO 


i8 


ooioviNMnioooMJoooiooos)'* 
>*^oorHiO'^Hioioaicoi,otO"i,coontO'-ico 
t^ooo-«fr|c©oo-<J<ooo©-<jicot^t^ooo 


lOioioiOHOonioi 

"  1  CO  N  (N  lO  m<  co  o  l 


CO     CO     M10OO' 


1-S^ 


Jag 


S* 


•CO  2 


ho 

O-X  Pi 

1st 


g^  g  g 

p   p  Or<      P,     Pi 


M§m  :  :  :w«^  £  »  :  :eat3sw  : 


e 

SP 

6 

p. 

t>> 

F» 

h 

fr 

to 

to    o 


Pi   • 
c?o 


IS 


O 

o 

o 

<<j 

*8 

<% 

o 

o 

o 

p 

p 

p 

BLATCHLEY] 


TABLES    OF    WELL   DATA. 


313 


coK 


-a 


coPh 


l"«M(NOOO 
NH001N(0"5 


ioi(NO)>>iaNNNni'r/-r( 


l  rt  r-H  CO  (N  <M  (M  <N        MNiOOOaOlONMi 


|iOOO< 


NM^Ot-i 


OOOOCOffiWOOrHOHCOOOCONcOIMtOrHtClOOO'*         hji  0>  OS  OS  t*-  00  OG  00  00         NXlOOOHnOOOt^O 

•*oo^HNtotocooo<o©ooo)MMOiomNio^t      t^coeoioiO"9"inocLO      co(M<Mcoi-i-*fiomc\i-»<m 

C<Ji0000)'<l'OMON«0>0»'-iN«0>0>'HTf(005   t-H  CO  OS  G>  t-h  CO  CO  «0  00   OS  i-h  CO  00  C3  Ol  »-<  C*  CO  tfS  t 


m  m  cm  oo  oo 


1 1«  m  w  n 


03        HHCOW        CO  id  CO  CO  CN  <N  tH        i-h        <M 


■*lOlOOP5M 


OOOCO       V!OOOM1«^(DSOOOC» 


D  P   £  ©  fc£  M 


o  o  ^  o  o  o  o 


o  rv" ^    •  <    3  ' ,/w  w  w  w 
K*2  "V  £  ?J2  cjc  be  be  tr. 


t5  £  _2  bo    .  £  ?  .2  be  ~  p      .2  be  S^  ?  °  fcx  b"  ~  %       t>  <2  be  %r  &  >  S,  be  be  be  b 

«   :MMScacat3    g  go  &£%  (apses-     ggco^M^iSccccpsc: 


<n  r~-  oj 

r-H  o  a> 


o  T-< 


o      o 


ft  ft 

s  a 

2  2 

5  o 


CO 

CO 

CO 

CO 

CO 

CO 

CO 

CO 

CO 

CO 

CO 

CO 

CO 

DQ 

8 

In 

85 

3 

o 

CO 

eo 

CO 

CO 
CO 

CO 

CO 

CO 

co 

00 

co 

OS 

K 

314 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spaxeq— }onpoad  p3i;rai 


188J— mdap  moi 


•183j— r^dap  uo 


c 

o 

I 

8< 


um^p  aAoq'B  opnii^y 


iCOiOHOlCMiOMOCiSOiOMHOjeiOMMOllOHOONHO 


•138J— I8A9X 

■B8S    A\ojaq    epn^i^xv 


OC  <M  (M  tj>  00  ■ 


tMCOCnOliONCOHNHfHM, 

O  N  O)  H  ff.  CO  iO  C5  i— i  OS  •— I^TfCJTrffir- ICOOOC01"N1000CC' 


S8SS 


paiBJiauad  ssau^otqj, 


•U5«ON«itC'*«t-HNCONO      'CT-C'^O      'lOOHlON 


i-l  1-H  I-l  •*!  «D  CO  l-H  ^H  i-H        •  CO  T-(  C$  irH 


i28 


■*  o  ■*  o  >o  «o  >o 


•;aaj— doj  o^  q^daa 


ir~'*'cDTfOOO-3<co- 


jlU 


02 


CO  !D  f  *  * 
<N  CO  CO  CO  CO 
1Q     U5     "5        O        iO 


■«»<        M     W     H 

6      6    6    6 
55     55   55   55 


C3  C8  C3 

.2  ,2  5 

Q  O  6 

o  o  o 

s  s  s 


55   55 


o    o 

55  55 


o    o  a    o 


55 

a 

a 

a 

a 

a 

a 

a 

a 

a 

a 

a 

a 

a 

a 

a 

o 

c 

c 

c 

c 

o 

c 

o 

o 

o 

o 

: 

o 

o 

o 

r- 

00 

as 

o 

OJ 

CO 

p<  • 

TJ1 

■f 

-sF 

Tfl 

•«* 

T 

C3  O 

S55 

1 55 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


315 


c 

i 

or 

ZZ  © 
13  © 

© 

*c3  : 

CO     . 

|i 

Oa_T 

CO 

o 

93 
03 

1 
It 

"r 
DC 

c 

- 

CO 

ooo 

r~  o  o 

,-tCMCM 

1 

£ 

g 

(N 

NO 
Ti-O 

o 

00 

1 

- 

CO 

c 

- 

QQ 

(5 

C  O  T  o 

1 

rr 

CO 

•  1-^ 

i—  s 

T  T 

CO 

o 

to 

00 

re 

OiO 
00  C". 

coco 

NOCO 
30  CO  Oa  T 
OaOCOO 

X 

Oa 

0«0  »Q 

O  T  L.O 
C  TO 

DC   Z 

S§3 

CM  CO  l-         O 

IN  ic  oa       ■- 

Tf  T  CO          T 

Oa 

CO  T 

L-0 

10 

K 

2 

T 

y 

r 

- 

— 

c 

i 

:- 

r 

1- 

p 

/ 
7 

a 
— 

OC 

c 
C 

—  — 

EC  ^ 

r~  i—  lo  c  co  co  e? 
--r  y.  o  co  co  •-=  _: 

UJ  lO  LI  O  lO  lO  i." 

— 
p" 

—  o  t^ 

CCC'X 
L.O  IQ  LQ 

N  — 

—  —  C" 
©  **•  T 

1-HGC" 

COTOCGCOi-icOt— 
OC  t-  irj  O  *Ji  tji  CO  CM 

Ca  f-  CO  0C  OC  CM  —  CM  L0  CO  —  CO  cr.  uo  c  r-  I- 


iOOCO         or.  ^Hi-HOOrH      00 


.ffiO)Olt»000!'-iO)0>( 


CM  CO  CO  CM  i-i  CM  CM  : 


CMC<iNL':NCMr;c--<cr;CNi-':rcc-Nccc-ccccicc' 
23  £r  3?  re;  2  2!  2!  71  ~  £3  rr  2  72  °  °  J "   ~ 


o  co  co  oc  oa  c  a  co  a  x  oa  cr.  x  i 


GlCtfCCO      CM      CXCZ^HMOO 

lo  lo  t  co  cm  —    -r    rc  -  x  l:  m  l;  c  z 
Tt^OCOCcaO    O    HNBi-LiiCijc 


#8 


o  o  o  o 

Z.  Z.  Z\  Z. 


hCncc-hCMcO 


o  o  O  O  o  o  c^  >> 

fl"^    CD    fll    rti    >n    ^    ^-i    k.     C/j 


o  o  c 
ooo 


a  •  &pM^^_  _  z+z-$    -ooc 

&b-m  So  w>  bo  a  §b  a  St  ?  °%  r5  ^  >. 


73  t- 

°  2 

o  ft 
J5 


.   to  6C  t£  CJD  ^   t£60i£cjccjOWtJC!>C^?|?-|S      ,      .OfS        -  f*6C. 

=  'OT3'o''0  c3t3'0'='c;73  --t^q  &■*¥■*  £•¥-  o  c^-^  c  a     rH«5  C 
3  "C  -C  -c  'C  O  "C  "C  "C  "C  t3  'C'd.HCC^^-'j-'it  p  .S  'd  o     rt  'C  ^ 


^'d  o  o  o  o 

.h  •!-"--!  rrl  T-!  r,-j 


~- 


Ig 

1=1  S 

C3  05 
-d  3  3 


rHCj)CO 

tJ'd'd 

ooo 
o  c  o 


CO    c^ 


<-l  CO  CO  CO 
CM  CM  CM  CM 
lO  lO  LO       o 


cm      co    ca    o    coi 


S    5? 


to    o 


6    6 

^   55 


o  o 


N 


—  o 


o      ooo      o 


^^A<  r^S 


^      ce  c3  c3 


55     ^     ^ 

^     t^     t^ 
©      ©      © 

a     a     a 

S        S        d 
'©'©'© 

GOP 


o    6    6     •  6      o 
55   fc   £   gfc     ^ 

^  >>  ^  ™r^     >» 


a  s  c  .s  q 


©     ©     ©    'C 

P   O   C   <! 


o    o 

3  3 

o  o 


c      ceo      o 

2    222    2 
o    ooc    c 


ooo 

2    2    2 
ooo 


o    o    o    o  o      o 

2  2  2  22    2 
o  o  o  oo    o 


316 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


•sjoxreq— ;onpcud  rei^rai 


•^aaj— q^dop  p^o  j, 


•^88j— q^dep  no 


T3 
CD 

.9 
a 

o 

o 
I 

55- 


•^98J— I8A8I 

■B8S   A\opq   apnmpy 


'WW— 


•^aj— do;  o;  q^daa: 


02 .2  ®  >.2. 


££ 


IOC3t^«D'0-<J"*rf<c0C0'^'ait^iC 


^NOOlOOffliOf^NOCSOONiOiO 


OOOOCOOOCOCO^OOOO' 
NvinN000)OOOHHOirjN0>O 


M00MN00O:iO0000'<J<N'*©rHrHCOtC'^r-l 

"        eiOHCOHMOVNOCiOHNffl 

N'O'iocoocsooNi'iotot^aia 


ifliOOOiOONiOMM 
^owio       hco  i-i 


lOiflowiooHiowiooioiooiOfiooNioiOHTfooiflooiniowo 
NfNcoHOOcmtDaricortOHTtKiooooiO'WOiNoiioafqiMNMij'rt 


o 

ft 


o 

o 

£ 

£ 

Si 

to 

a 

PI 

M 

M 

ft 

ft 

o 

d 

O 

O 

W) 

tun 

fl 

C 

c 

PI 

I 

ft  • 

03  O 
S     . 

33  o 


«     rt 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


317 


38 


*j  - 


co  42^3^2 


R^ 

■  d 

•■A 

■  a 

03  c3 

>J3 

Sfl 


;8gg  :8 


»C     •  t>-  Ui 


qo      «  a:  t  io 

CN        m  CO  CN  <N 

00        to  CO  CO  CO 


S3S8 

tC»0 


OS        C  C  OS  CS  < 
F-       to  to  uo  iC  < 


OU5        O      •  lO 

to  to      lO     •  iO 


HCtOHHHTfNl 


COOrfMHrHNOOtDNfOiOO 
NNOM^OONN^KOOMOO 
iOiOMOmiON®iOiONHHN 


C<5  (N  N  V  (N  rr  rf  NNOV(DMOO>  00  00  i-l  00  CO 
NNrtiOUtCON  iHrHCOVNOHTr  OONOOO 
TJi  CS  t~-  UO  ■*  CO  CN        rr  Tji  TT  ^*i  t}<  CO  Tt<  rfi        ^  Tt<  r}i  to  >0 


.  (OOOHOSO 


r^Trtor^cs05co<N'<J"OctcOioo 

I>.Nat0iC03CNN00rtlNO(N 
CSOS'-i'*t,OsOsCNOO<J3CseNCOCOt- 


t^  00  00  to  OC  to  to         OC'CTCtOVNOH         CN  CN  CS  CN  ON 

cn  <n  oo  ■>*  •*  eo  t»      wocNicNcosio      HNoao 

OiONOSOwM        OOOOOi-iQO       ©  O  O  00  CS 


COCOCOCN'T'CO'^'COCN 


NNlOi-ICOrH 


'  lO  t>  CO  ">*<  lO  t-  00  00  CN        lO 


00  O  O  00  O  0C  CO        CCI-NL-XNW       ootowio 

-3<  t  o  io  (o  'r  rj      ococa-  vnoo      ^  ©  tj<  tt  •<*• 
is  o  co  ^  io  c  i'-      (OfflLcicccccio      io  to  >c  f  io 


■  C3  03     •  O 
n  O  O'S'S  C3^  o  o  o  o 

P2  :  :q3cq-  m  :  :  :  : 


■a  IP 


CT-  C  O   c3        O 
7?  irt  irl  -3        ^ 


III  jl  II 


P      i      ■      ■      .  <D  P"     i 

^  o  o  o  o  «t?  © 

M  :  :  :  :eh«  : 


T1^ 

o  o  o 

o  o  o 

SSS?0 


I  CN  t^  O  •<*<      CO         CO         i-l         CO 
CO  CO  00  CS  O      CS         CS         O         i-H 
■     -^       -qi        iO       lO 


lO  lO  lO  ■*  ■ 


o©  n 

uO  uO  L-, 


N(NN-     .-c 

HHHM       TF 


ss? 


00  t-  CO 
CM  CO  lO 
iO     iO     iO 


CN  CN  £  00  <N  r-H     CN        f~        ^        CM        CM 

ooxoooo      o      6      6      6 
fcfcgfcfciz;  £    Z    £    z    £ 


.sagesa  a 
wa§aaa  a 


a   a   a   a 
a   a   a   a 


o 

o  o  o 

o 

ft 

^^^ 

fc 

>, 

>>>s>> 

>> 

£ 

^^3^1 

^d 

03 

c3 

PI 

Sap 

fl 

0)     QJ    © 

CD 

.O 

^^rO 

^2 

-< 

<<K 

<J 

0,W^^«M  M     W    W    M     W        i-J 


■^  to  oo  to 

<N 

t-^H 

l-H 

CO 

CNf 

o  o  o  o 

O 

o  o 

0 

o 

o 

^^^^ 

fe 

^^ 

53 

» 

z 

>>>>>.>> 

P. 

>.>s 

>s 

>s 

>> 

^X^^l 

A 

^^1 

A 

fl 

-a 

-1 

C3  C3 

efl 

en 

cfl 

a  a  a  a 

fl 

PI  PI 

3 

s 

g 

JB 

,0,0,0,0 

- 

^2X2 

rO 

^Q 

-^<<< 

-4! 

<5<1 

< 

< 

< 

wmmvi 

CO 

CCCQ 

o 

o 

0 

-^oooooo      o      o      o      o 

§32323  3    3    3    3    3 


o  o  o 

a?©  e? 


o  o  o  o    o    o  o 

3333  3  33 


o    o    o 

3  3  3 


u 

UOOOOO   o 

O 

o 

o 

O 

m 

oapopQ 

oq 

oooo  o  oo 

O   O   O 

-1 

OC  Cj  O  -h  CN  CO      Tf 
^^-CN  CN  (N  05     IN 

3 

& 

in 

S 

CN  CO  -^ 

•o 

to  t>  OC  CS     O     ^H  <N 

CO     ^i     "5 

318 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


•sjaxreq— ^onpoid  ibi^tui 


•laaj— q^dap  r^oj, 


s-  o  o 
o'C'o' 


CO 


'laai— q^dap  no 


lO  lO  Tf  Irt 

UO  lO  lO  lO 


CD  in 


n3 
o 

o 


um^p  aAoqis  apn^x^v 


iNHiOt^ 


3S 


HinoCMM 


cococoioioiocoioeoioiococoi 


•^09]— I8A8J 

■eas     Avojaq  epn^T^xv 


pa^a^aned  ssau^orqj, 


■^aaj— do;  o;  q;da<i 


3   O   ©   53   fl© 


O 

1 

C3 

rfO 
S2 


•rt  o 

CO 


OOOOO 


Oi  00  CO  Oi  ■*  00  i-H  i-H 


NO'^'l'^OCOlTliOtOtOOOCON 


COCO<Ni-Hi-l 


OOOOiOiflHiOOl 


iOOKJiO 

ION        i-l 


^ifOOOlHiOMOOOON' 


io  io  ■*  tC  CO 


Oi  co  coco 


CO  CO  CO  T)i  • 


\ii 

•  o  o 

:££ 

.S'd'd.b.S 

W  :  :{2m 


I  O! 


£  c3T3^T3  C3QO 


££   '.'ZTo    • 

-tS-S    •  o  o  o    •  o-s  o  o 
So*;  £££-„£  o££ 


o££ 


N<*     O     NcOw     CO 


co      >n>    co    co 

CN        NOW 


iH,-ia> 

P    o  o£ 

6 

6 

o  6  6 

6 

6 

6 

6 

o 

*"< 

1-1 

o  o  o 

fc 

vt 

£ 

£££ 

14 

fc 

£ 

B 

fc 

o 

o 

£££ 

-3  ^*e« 

c/T 

B? 

DO 

c/T 

14 

14 

bern 

son, 
mel, 
omb 

P 

,fl 

,0 

,0-0,0 

,o 

P 

P 

P 

P 

aaa 

S 

3 

o 

aaa 

o  o  o 

a 

O 

a 

o 

a 

o 

a 

a 

c 

a 

a 

aaa 

<«J  |So 

o 

o 

o 

OOO 

o 

O 

U 

u 

u 

a 

a 

Ph  Ph  hh 

co  q'Mw 

M 

w 

w 

<<< 

H 

H 

w 

a 

H 

a 

6 

-  % 

OOO     o    ^  o  o 

333  3  o33 
OOO  o  §oo 


d  a  g 
"3*3*3 

O        O    Q,rt>Q>     o        O        OOO 

3    3    ...  3    3    3  3  3 
o    O  OOO  o    o    o  o  o 


COt^OO      »-H      tN  CO  TJ1      lO 


t»     000)0     'H        <N         CO 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


319 


© 

o  ®  © 
-d>2<2 

ChO 
C3  o  O 
^2  CO-* 


■-    71    f! 


en  d 

CO  o 

.-H'-d 
d 


(3  e3 

GO    .CO 


it  ri   c3      t^  t>. 


8  :88 


gg 


o    '-ho 


OOffliflONCNOC 
0>0>OC5'"1,«)O00Otji 


O      •  O  CO  O       •  <M  LO  CO  O 
CO       '0)^0       'MINXH 

tk    -oooco    -oooocnoo 


occ^ocl-: 


.-h-hOOOOO'-K 


)  CO  -r  —  <N  tt         (NiON 
_    _  J  O)  lO  ©  N  O         LOWO 


iOM^it-<0  01(10  00MNfflmOtD*OL'>N2COOH«5MM»«Nr- 

KjTfOHlOOHNOHONOHOHOONOHHtSlOOVHlSO 


O        00  L.O  CO 


LO«OMOHNCSlN^-rNC---^"'-l-3r.'r«NlMN3:M 
r3INXN»0^r:iOOCOrtC:XML':cC.CHCCNTfNOIMNTl< 

oo^eoooococ<i-*co^c^-^co^cO'«jiT)<cN'*}<eocoooc5cnococn''J1 


NlOOJt^-H 


c^S^SSSSSSS^SSSSSSSSS*9  :^22|S8 


N  M  O  OC  '— iTN»- <01H  /  N  ^  N  O         r^CO»-i 
OOOOfflOOCOnWOOOOVfflOO'J'M        *Ti  uO  t- 


M-HNrtOswNrtOOC:OM 

n<i-oaiooco-^"00ooor~cnr~ 


CC-.NONPCH 


ohock^c-oz  c;  ^  >-~ 
0000:Ot^Oit>-OOco-*rriTft^cOC5 


T5  O 


O  O  o 


O  O  O  O  o 

PhPhOhPhO 

©  ©  ©  ©  k. 
hr  hn  hr  fcn  > 


:^p,§ 


©  ©  ©  S    .  cq  ©  >- 
•Cd^'E  "C -5  ^  'E!  "C  "C  -C -3  i  o "fl -~  O 


is 


.  & 

te  >.© 


o  o    ,  o  o 

o  ft  .  o  a 


©tC.^P-bc.P-bn 

S^  O  "S^d  C^'O'  OOOOOOOOOO 

m£m  :s  Mm  :Wca  :::::::::: 


o    w    «    (Moo    o 

(N     <M     O     Oi-H     —I 
lO     lO     lO     LOO     IC 


(N        C--  CO  • 

lO        lOOi 


8  2  8 


O     00     M     00 


COO     00     <N 

oo    o    r- 


,_!       ^H       <N       1-H  <N 

666060 

55  fc  fc  ££  fc 


000 


s  - 


O     t—     00 


s   s   2 


<NCO     O     00 


£  £ 


05   ©      ©  © 


g    g    g    gg    £     £       £     £££ 

g  g  g  gg  g    g     g    ggg 

5S5  S3  3   2     2   55S 


g  g 


d 

6 

6  6 

6 

6 

6 

6 

6 

6 

6 

6 

0    6 

6 

6  6    6 

6 

w 

fe 

££ 

» 

B 

fc 

£ 

z 

fe 

53 

fc 

Z   5? 

s? 

ZZ   » 

fe 

c 

u 

1/3    w 

B 

b 

B 

00 

M 

?:< 

s 

^r 

s 

tJO     bX) 

B 

txS)  S) 

B 

u 

ex  tx 

W) 

u 

bn 

M 

u 

bi 

W 

u 

M     tX) 

M 

b£  W)     &X) 

u 

O 

*C  'C 

B 

'C 

C 

■c 

"C 

•c 

•ej 

'C 

s-     u 

s 

c*c  c 

"C 

0 

CO 

O 

C3 

r 

0 

C3 

CJ 

0 

0 

O    O 

-J 

OC   O 

0 

a  *-d  a 

000  00  o 


00c 


000 

aaa 

000 


o    o 

a  a 

c  o 


^2    o    c  o    o    o    o 

v<«  a  a  a  a  a  a 

w  O  OO  OOO 


0000 
a  a  a  a 
0000 


0000 

a  a  a  a 

00  o  o 


?5cn    c5      c5 


I  cq  CN»      S    c* 


!N     CO  •"»<     tii     CD 


(M    co    -r 


320 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq— ^onpoad  i^i^ini 


•}8aj— i^dgp  p^oj, 


•}99j— t^dgp  uo 


ranji3p  9Aoqi3  apn^i^v 


•198;— I8A9I 

■B9S   Aiojgq   apnii^v 


•^99j— do;  o;  qidaci 


1.2  ®   ^.Sv 


53* 


•J3  o 
to 


S8S 


Or-HOO 

OHlflrt 
00  C5  CO  00 


C3  a>  so  0>  00  - 

OHfflHQOl 


iOS<N  0(MO«5> 


0>«OOHO!t>MMNNOt 


H  lO  O  M  M  Ci  ( 
liOO*!OON( 
i  00  CO  iO  00  CO  iO  < 


I  00  COTP  00 


-c*iO'OCOOOOiOiO< 
r0<£>O<NC0OC0<N>0< 
OOCT>-^COCOOOOCOOVOOO< 


O  lOOs  CM 


HNOuCOlOO^N     -    - 

HTfOMfoCHocor-omoiH^ 
oscoooocor^ot^ot-ocot^-Cico 


.'d  u    ;   ;    ;   .'-^  t-.    .  ^  t-. 
.  o  o    •    •    •    •  o  o    .  5  o 

O     •     •  Pi    •  O  ft     •      •     •     'Oft    'Oft 
r^OOdOr^dOOOO^dO^'dOOO 

t  d  d  -c  d  £  -c  d  d  -d  d  .£  -c  d  £  -G  ^  d  ^ 

j  :■  :pq  :^pq  :  :  :  :^m  :^w  :  :  : 


:W 


•  be    .  > 

;,d  eg 
"  'H'd.s 


32    8 


io  io    io    ■*  ■ 


rf    <o    io    <o    ic 

»     Ol     SI     M     00 


00      H      O      rH      lO 

•      6  6    6    6  6c 

o    o    o    o    o 

o 

c    o    o    o 

:     ££  5Z 

££  5z 

5Z 

5?  £ 

£  z 

55 

5z 

fc 

/ 

55 

34" 

rt 

,d.d 

rt 

■d 

d"  d 

^T 

£ 

,d 

d 

,d 

£  ^ 

61) 

SjO     tX> 

bx 

60 

u 

fl  d 

d 

p 

d    3 

a 

d 

d    d 

fTt 

03  03 

ftS 

09 

03     03 

ffl 

S3 

efl 

crt 

SJ 

03     c3 

T)T) 

d 

dT3 

Tl 

■d 

d    X} 

d 

^ 

« 

•d 

d 

•d    TJ 

dd 

d 

dd 

d 

d 

d   d 

d 

d 

d 

d 

d 

d  -d 

5353 

£ 

£53 

53 

£ 

3  53 

53 

53 

53 

a 

£ 

S  * 

o  o    o    o  o    o 

a  a  2  a  a  a 

oo  o  oo  o 


o    o    o    o    o 

a  a  a  a  a 

o  o  o  o  o 


o    o    o    o 

a  a  a  a 

o  o  o  o 


55     fc 


BLATCHLET] 


TABLES  OF  WELL  DATA. 


321 


©  «  o 
a>  ©  o 
'—'  ©•<-' 
O  —  r- 

i-T   _(-T 

©  cr<0 

"t^  ^  ^ 
|  W>« 

>    Q    > 

SB'S 

03  O  03 

to  coco 

© 

o 

lO 
lO 
CO 

09 

O 

© 

(X 

© 

CD 

"3 

«2 

M 
DO 

03 

c 

-0 

a 

CS 

CO 

§ 

jfi 
it 

© 

O 

03 

o 

c 

K 

C 

o 
to 

O 

O 

r^ 

ifl 

DQ 

,4 

o 

>o 

iffl 

o 

i 

1 

1 

1 

K 

00 -^ 

-T 

a 

■ONOOOilN^W-HMtOpHOOKNG  I 


HrtOC't^"©NONHOJN 


IHftHHONi 


0"*'HOOffiOMOJHNHWC11'rtTliO(NNP3(D 
Oi(OiONHOiNHa01HOOO<0!0>ONHONH 


i  O  Ci  CT>  CO  »C 


NHONOMCOOOCO        NNmOl 


■*(DOiO:INCO»"MO(<OSHOOi 

OiOCJltOOOCNCOHrtlOOOlOOl      - 

ICC'J<iOCt»XCOMOM?5^(NC<:iOiOiOM©MMiOINCOiOtqM'*iOOOXOOOlN«l^«MM'* 


OOOOiOOOM 
OWIOOION 
(DNOOOOO 


)N(DiOH©05NNOCOiOffiiOO«00 
I        CNCNCNcO        <M  i-H  <N  i-H  iH  CO  tN  i-H  i-H  r-l  O 


oo-^iot^ooo 


ooo  mo< 


iU500'OiC!»OiOOINiO*0«NOiONOOW'*ON 
>««0000O0000»NMOOrtM 


I'O'ONOOHNOOOOIN        OOOCWOOi 


oooooot^oooocoMTfTtiNooat^i 


t)ooo' 
'C*3  did 

cq  :  :  :c 


.'rt  t- 
'  o  ft 
!#T3  o 

Wee  : 


o  o  o 
o  o  ft 


■c-c 

o  o 

:   c 


o 

■  ft 

>»>»>>© 

>  >  ©  m 


:  :  :  :  >>£  £  &  :  :  :  :  s  &  :  :  :-w  ?  ?  ^sb  :  :  ;  :  :  :  : 

OOOOaJ^-^TjOOOC'S'dOOOoS^'^S'^OOOOOOO 
TJ'^'O'C!  s- .^  .£  %~  T!  T>  t3  T?  3 -£  T3  T?  T5  ^ -^ -^  g'n'O'Cd'd'O'd'd 

•  •  •  :pqcq  :  :  :-  ww^pq  :  :  :  :  :  ' 


03*  C3^ 

to 2  Mi 


o 

o 

0 

0 

£ 

£ 

53 

fe 

CO 

a 

a 

a 

a 

,§ 

44 

M 

M 

M 

PQ 

rt 

c 

'd 

-o 

'■£ 

* 

a 

C 

a 

P) 

Pi 

fl 

Pi 

PI 

d 

to 

to 

to 

to 

to 

to 

to 

to 

to 

t~ 

oc 

OJ 

0 

_ 

-r 

3 

OJ 

<N 

—21  G 


322 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,      [bull.  no.  22 


•siaxreq— jonpoad  im^ui 


•}88j— mdap  ib^oj, 


^oaj— q^dop  no 


■OOOO 


OOiOiOOiOiO-^OCMiOCM 

SiOOOtDMOiCO'^OINtO 
MOC0  00  05  00O05OM 


"O 


wO 


O 

T 

o 


•}99J— Q\XB\d 

ran^p  OAoqe  gptnpjv 


B9S    Ai.opq    opnmjy 


pajBj^uad  ssgu^orqj, 


•}99j— do}  o;  r^dga 


tf  o 


•rt  o 

Xfl 


OOOOOOOONO'OCCi 


OiOMCCOrHiCNNOONNiOiOMOiO' 


ocooooocoi 


CO"*'^<OO^OOCO-<tlCO^C«5Tt<OOCO,*lO< 


nDTr^cot-nocotooooiooooi 
iHeo«HMNcq«HWH««i 


I  CO  CO  00  CO 


<-H  CT>0 

00020 


CO  o>  CO  00  < 


'ONiOOHOO 
iNMMC»t^t» 
I  00  OS  o  CM  CO  "* 


pq  !  :pq 


SSpq'Sf 


fe.  ©  >  a> 


•d  £ 

•  o  S 
i  o  Q< 


^o^'O^'dooooo-^'dooooo 
3  d  .h  •£  .3  '£  d  t3  d  TS  d  .55  T!  d  d  d  T)  T3 

:  ;^pq^pg  :  :  :  :  :Mfq  :  :  :  :  : 


rji     o     O  ^  "*>  lO     iO 


^6    ^    odod    d      d 

ij)   q)       q}       gj   ^)  qj   qj      q}  q} 

PmCm    Pm    FmPhCmCm    Cm      Pm 


pq 

pi 

<» 
•d 

£d 

§£ 

coO 


pu   Pm      Pm 


o    oooo    o      o 

3  2222  2    2 
o  oooo  o    o 


o  o 


I  -  A       35  O  ^H  CM  CO   -P 
CM  CM   CM  CO  CO  CO  CO  CO 


BLATCHLETj 


TABLES  OF  WELL  DATA. 


*~ 


u 


g§ 


3§ 

si 

0*f 


H 

©8 


02 


£  :£ 


<NOOC  iOU50(0(NHTj>0)'!fO)0> 
OHNONiOMHiO^OXNOiOiO 
NHO>MHOO)NCOOHHH005 


C*»  OS  05  ^  OS  Oj  t 


IOO< 


lOOiN        HOHO«D«iOiO 


iMOKJO 


oooooioioo^oooip. 


I  00  CO  CO  CO  **  lO 


a>osco^n^o>-ir-Hr^.too5ao 

(NiO00NWO5O5COMiO(Nifl 


IHNHHCOMCO 


it^OOCJ        iO  l~-  00  O  O 


NrtOiOOiOOtOO)HU5t>iONiO 


!S8 


iO»-l        .-I- 


ig88§882    SS3°°S 


oooiooioioo^oooioomoo 

r-SS^OOlO<N»OCO<MCOOOiOl^-<M<M 

r-oooc^oociOiNcocor-oo  — 


00  00NOOW! 


CO  (M  00 

OCO(OlOlONN-*H«IOC<5 


O<N00OOi0<M<M 

HMOOW00NN 


-o  o 

w  : 


'O-" 

:*  M 


)  o  g 

!  °  & 
•-"CO 


C3  g     •  O^C^CO  E7° 


_3  J5  03  K  ©  ©  ©J2  W)   . 
-CdtJ      3  SO«  2  2  2  o'CcJ^o 

mod-  meh^hScq  :  ::     pq 


tuO    . 

•dooo 


5     * 


•  f»  C3 

i&j 

Iff 

cS-^cQ 
^pq 


1 

p 

fas 


c 


Wh 


o 

o 

pq 

pq 

d 

pi 

73 

-o 

£ 

► 

PQ 

pq 

pq 

pq 

d 

a 

a 

« 

oj 

<o 

<o 

ti 

-a 

>d 

-d 

£ 

£ 

£ 

£ 

o 

o 

o 

o 

0 

fl 

a 

0 

02 

02 

02 

02 

324 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.    Tbull.  no.  22 


•sxau'Bq— ^onpoad  lejjini 


•}99J— md9p  1T3JO  J, 


coO 


ta     ^ 


3     S? 
co     WO 


•*aaj— mcfop  no 


PQ 


•}99J — QWB\& 

ran^p  gAoqe  gpnmjv 


l  O        OS  t^-  <C  iO  ""J1 


iOOIhONhh        0)N!0"OiOOffltO 


•}99J— X8A0T 

■egs   Avopq   opn^i^v 


CMCO"^       ONOOOO       CO  Tji  lo  eo  tp  CM  co  co       uo  l>00  Ci  OJ  ■*  oo  ©> 


§£; 


•}98J— 

pa^BJ^9ti9d  ssgu^orqj, 


i  LO  CD  00  O 


IMOOOOO( 


'^99J— do)  0%  md9Q 


_      JOQO        OOfflWOJOCOOO 
_      JO00  y-t  -H  TH  O  0>  CM  O  t*  CD  00  lO  T}i  t~-  Tf  CO  CM 

t^OOOi         OCNCO^IO         00  Ci  O  00  00  «>•  00  00         O  CM  CO  Tjl  ktfi  05  CO  "«< 


M^   m    ^   ^   0)  Mm  I* 

OOOOOO^^S^O'O^ 

^^^tjt^-chQo-s-"  2'no-- 
:  :  :  :  :  :pq    -  mMhcq-  m 


g  o  ©  c3  a© 
co.2  «  >££ 


S£ 


23  o 


a 

.  a 

a 

a 

a 

CO 

CO 

CO 

CO 

CO 

_l 

<N 

CO 

-*l 

BLATCHLEY] 


TABLES  OF  WELL.  DATA. 


325 


•fe  : 

>' 

)     • 

tH 

«£   ,<?i.  ■ 

l~ 

CD 

<2 

:j£  : 

:©m  : 

0 

0   .-1    . 
§  :-«  : 
-r  :§  : 

-d 

1  ! 

»o 

~~ 

S2    -o    . 

8      ,t»      , 

00 

so 

•  ^4~CD      • 

:  ~£-J 
•  ^^^ 

1 
3 

.a.' 

CO    • 

2  :tS  • 

a 

0 

«8 

so 

BO 

10 

O     ; 

I  : 

rt 

"5 

£ 

imes 

alt  w 
feet 

09 
O 

^ 

r-1   _,_ 

..  8 

"el    : 

DQ 

0 

IraC 

UJ 

3 

j  :a 

CO 

K 

X 

C3 

CO     . 

c 

0  0 

0  o.a    .  O 

«o 

1- 

5 

10 

CO 

s 

0 

,e 

^543 

DC 

COCO 

COCO         ;co 

g 

= 

CN 

'- 

O 

<N 

- 

-r 

1-1 

M 

1-1 

1-1 

'""' 

1-1 

a 

R& 

as  0  os  cm 

lO  00 
00  00 

a 

100 

VICKOO 

CO  tj 

rtH 

-"-'*«'-< 

rt- 

OB 

r-H  1— 1  >— 

iooo>oiNiow 

OOlNOOlOO 
U5HHHO0100 

i>.  tji  co  00  i>-  as  a- 

00  H  O  rH  CD  00  <N 

tO  ffliO  ■*  C3  H  C 

i>--Hasoooooo-<fCMr^cNt^oc 

MflO 
COOCM 
CO  >-H  CO 

CM  OS  lO 

r^a 

OrtNCJOOHOOOOHK 

.  »-l   Tt<  CC 

CO1OM1- 

CO  CO  lO  i— IOSCOCOCNt-IOSCOiC 

iHOJO 

rt 

'H 

,-!,-.  rHrt 

r«»H 

i-H                         riH 

:rt 

1-1 

T-*rt 

7-<    -91 

00  co  t^  a- 

COOS-HCNCNIMCOOOCOOOCOCN 

.  t^^H  ^H 

co  >o  0 

00  ^H  lO 

t~-  00  lOr- 

I--  ■*  1- 

hoooiooohn      ooocMcocooooasasi-iooT- 

.  00  10  co  co  as  00 

00  OS  i-H  CC 

CCl  10  oc 

as  co  co  co  *>*<  »o  co  00  00  as  ©  t-i  co  •>*<      00  00  as  co  »o  00  00  cm  co  10  00  a 

■  co  0  00  00  CO  00 

"-■ 

HH 

CO 

iO  CN 

OOOO 

■    .10 

CO  iO  lO  O  CN  10  CO 

co  os  00  as    '.  0  c 

OUSlMOiOOONiOOOM^- 

.Ttitooc 

.CNOO 

CN  lO  O 

COIMCO 

c 

OM 

r*-  »o  0  c 

sss 

CO  iO  iO  OCO  O  CM 
<M  CO  iO  CM  CM  t^  <M 
■^  00  00  CSOO  CM 

OOHNNOOOO 
MHlNONf  C 
WfiOOOOOO 

cNoooooo-^oiooocr 

■  OOOMiOO 

22£ 

a 

O  CC 

-C"  ia  cooc 

OlO  CC 

COTf<TtiOOOCO-<f00050CO"* 

■  00  O  CO  CO  OS  CO 

ooaso 

,-1,-H 

HHH 

T-l  y* 

rH                     1-K-I1-I 

,_,  .-M --H  ,-H  T-l          tH 

HHH           •"•!-•«-•                  rtHri 

.           rt^H 

pH        rt 

1-1 

^  : 

p 

4_ 

M 

pi 

o 

0  3 
®£3~ 

-0 

0 

H 

O 

0  0  g 

11 

0  c 

!  0 

•  ft 

O  g  O 

>  asjrj  bi 

'-■ 

. 

Gas" 
irkw 
racey 
cClos 
cClos 
ridge 
do.. 

~m£i 

J:  ^ 

s 

^g>^ 

-c 

■°,2  § 

O    O    03 

<*X}  OOOOd 

d^'OoW'Ooo^ 

:-0  0  c3^Jn 

X)  O  O 

•nwo 

TdlSO 

.-1  "£,  ^  'O  T3  t3  £3 

rn  -=3 .53  -£  "d  0 .53  "C  'O  TJ .33 .33 

••s^o 

•33-n-a 

•a^-o 

ffl 

eq    2 

MB§« 

:  :^ 

Mca  :  :  :  Ioq 

S   W^SSfQ 

-  WWm  :-  Mm  :  :WW 

:m  :- 

WCQ« 

«  :  : 

o    o 


CD      CD 


fl 

a 

(3 

^3 

^3 

A    a 

^5 

^3 

CO 

CO 

CO 

CO 

0 

0 

O    O 

O 

O 

O 

lO 

CO 

t^ 

00 

OS 

a 

-H      CM 

S 

CM 

lO 

326 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


T3 
CD 

0 

PI 

•i-H 

o 

o 

i 


Remarks. 

1 

8 

1-1  a 
ft 

5 
SB 

co 

co^ 

C9 

0 

CD 

•spjiBq— pnpoad  iBtjtui 

•?88j— mdap  rejoj, 

* 

§ 

IcM 

CO 

OS 

o 

•CO 
•  CO 
•O 

.OS 

io 

s 

•^8j— qidap  no 

COO 
CO-<J< 

tO  H  CM 

00  0)0 

o    • 

So  ; 

•  rt<<NO 

•  CO  OS  CO 

•  ooooo 

CO 

00      • 

t>.    ■ 

:^8 

•  ooo 

COCO 

*d 

§ 
oq 

•?89J— 8UBld 

run^p  8Aoqi3  apn^iy 

iHHC0M"0O'0'*0010!0(N'*N'*<OH00iHNrH(0»0l0)OC3MM©rH 

!0'<tiO!»HOiONO)Hffl*iO'*HHHlNHHINSHNOOOMO!0'«'M 

H0)N®<DCqHH0>(NHHHHH(NN!0NHO0)NHO01H0)N!0e 

•^88J— J8A8I 

B9S   Avo^q   epn^T^v 

010>NNlOO'0<ONiOTt<OOtOOOCOTJ'0(NO)Mffl'fl<r- 1  .— 1  .— 1  Tfi  t~-  r~  CM  -<J<  O 
P3l005rtOOO-*NOOOOHijilOOOOOOONMOON(NOOt^O!H!DOO>intO 
C0Ol^0000C0C0C0OCMC0C0C0C0C0<Nt^00<NC0'«*''0<NC0''J<>OC0"0r^-0000 

pa^Bj^uad  ssauipTqj, 

OOOC    ~    S.    /C""O-:ii.,;i»OH00!0HO')"ill0JM«(DOOClHWffl 
l>CO        t-H  !M        .-1  -tfi  <N  i-H  TT>  i-H        i-l  CO  CO  .-H  <N  (M  CO  CO        CM  CO              T  »-(        i-l 

cs 

•^88j— doj  o?  q^daa: 

000000«5Q»OtONHO,<»,N'*N«NOCHOINNiN(N(NiOOOiONO 

■VfflOlHOOOVNOOlr-lNiOtOCofflOOOOJOOaKNNCOOOOfflOOOTlitO 

(»ocMcocoooooooot^oooooooooot^cscot^ooo50c^ooo50ooo<Ncoco 

I 

•J  :;■!■■'  :■'••■'■':  ■  ij  ::::::::  ;  i-?0? 
t-j.'ir^'g:;::;;:;;;^!;,;;:;::;:::^^ 

c    .    .    .  5  o o° oo 

ft  •    ■    'Oft oft *oo 

<v    .    .  ~    >  o :  :    t>  o j    >  t. 

bfl    ,  k^  P  ho ^j^W) ^i's's 

'OoS'cJ^'OOOOOOOOOOOoj^'OOOOOOOOOOS^ 

n  :S?Mm  :::::::::  :=  Mm  ::::::::  :^WM 

Sur- 
face 
ele- 
va- 
tion— 
feet. 

■ 

-HO                             CO                         00                   CO                      >-l                         CO 
O                      O                         O                      O                O                   O                     CT> 
lO                       lO                           O                       *0                 lO                    ""J1                       "^ 

"3 

*3 

g 
ea 

c 

c 
"c 
a 

c 

;          sz 

'c 

g 

1    l 

'             a 

•<3 
C 

)                  C 

;         jz 

1                £ 

t 

c7 

s                a 
5                c 

1               & 

>> 

a 

03 

1 

o 
'3 
"3 

I 

> 

1 

> 

Is 

3            S 

> 

K                   - 

r 

Is 

Is 

!               ,£ 

n           e 
i          > 

n              c 

:                 E 

< 

ft  • 

03  O 

C©                         l^                             00                         OS                   O                      i-H                         <N 
CM                       (M                           CS                       CM                 CO                    CO                       CO 

§   . 

23  o 

GO 

J, 

CO 

BLATCHLEY] 


TABLES   OF  WELL  DATA. 


327 


c 

0 

N 

T3 
CD 

O 

a 

03 

.o 

CO 

O 

oo 

r/T 

o 

CD 

o 

o 

o 
l~ 

00 
03" 

53 

0 

■S 

1 

§ 

OS 
of 

c3 

o 

+3 

09 

a; 

o 

s 

03 
O 

I 

O 

8 

aS 

o 

— 

3 

S 
~1 

~ 

OO 
00  o 

oo 

CO  0> 

oo 

C5CO 

o 

o 

o 
o 

- 

o 

o 

lOOO 

t-  r-  oo 

8 

CO 

oo 

CO  05 
OM 

X) 

oo 

M 

•CO 

•  oo 

•CO 

oo 

->cH 

:- 

- 

SI 

t^ 

I- 

00 

CO 

— 

OOOiOtOiONMCDNC 
OOiOOOOiONOO*MH(C 

i--  o  t~-  a>  oo  co  t~-  a>  t-  en  cc 

■-  ~ 
00  t- 

O  O  CO  O  CO 
O  CO  iO  ooo 
00  C3  00  oo  o> 

000*OOiOOO(OiON«5 

C»Cqt^OrtOOrH(NlOCO>010 

M^OOOOONOOOOOOIMO) 

oc 

T-HOt-o 

CONNN 

oo  oo  r~  oo 

lUJINOlOMHKlOt^t^CqtOmNOJiOCOMHHNlOOl 


i  oo  iO  CO  CO  CO  >o  00  i 


I  CO  00  Tf  t*-  CO  t 


Oh-NOiacOlOi 


iC0f-0000c0C0^OC0CNOC0^0000C0^C0^00(NC0CN^C0-^<C0C0-^-*l00OC0CN|lO< 


■  oocomooiO'j'NtD^iotio 

iOi00003tOO)0)0)NO)0000 
IIOCOCO-^CO'JIOOCO'CCCOCOCOCO 


INtDiOtOcOcOiOOOHUJNOOOt 
.  U0  >— IO>i0^t—  00  CO  tN  i— ICOOO-^ft—  o<  -  - 
•  00Ot>.CNC0C0t>.000>OC0t>.Ot-a>C0c0l>.C7Jl>-CT>C0l 


WOOMNOO!D(NU3lOOOO(DlOlOlOONOHONO 

..    jioooooHosrHior  • 

•CTsr-CTSOOt^OTCTJCO-^OOl 


o  o  o  o  o  o  o  o^Mt3  OOOOOOOO  O-^'O  ooo 
rT3fOrO'rOrOfd,T3rO.^.-H"£rOrOr^JrOrt3rO,drO,0,.rH"£rO'dfO' 


oo    oo      r- 


.-H  CO-^^H  i-H  0><Nt^ 

i-      coa>o      o      r^    as    oo    oo    o    o 


■*     ^     IO 


•"CM      iO      lO      lO 


VI 

2 

w 

w 

rS3 

O 

02 

CO 

rf 

p 

i-i    tc 

CB 

ir 

r-1       i-l       CO       .-H       H       ,-1      t- 

1-1    c 

c 

C 

c 

O     O     c 

C 

O    O    o    o    o     o    o 

c 

£ 

IZ 

£ 

£ 

2 

tz 

fc 

!z 

fc 

fc 

£  £ 

fe 

£ 

iz 

t^ 

CO 

oc 

<T 

c 

K.-rf 

5  I 

si   •d 

|S 


,d     ,d   ,d   rd   ,d   ,a   ,d   ,£ 

bfl        M     M     M     M     M     M     M 


S      S      S      £    S    S      §      ^^^S 


o 

o 

o 

o 

o  o 

o 

fc 

fc 

£ 

fc 

££ 

fc 

a 

PI 

PI 

a 

PI  PI 

d 

o 

o 

o 

o  o 

PI  pi 

P) 

PI 

fl 

q 

Pt 

rt 

rf 

.d 

3 

,d,d 

,d 

o 

o 

o 

o 

o  o 

,d   .d    .d 

OOO 


CO     CO        CO        CO 


o  o  o  o  o  o  o 

3  3  3  3  3  3  3 

o  o  o  o  o  o  o 

iO  CO  t-  oo  OS  o  >— i 

■*  ■*  Tf  ■*  TJ1  «5  lO 


o    o  o    o 

3  33  3 

o  oo  o 


328 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


•siaxieq— ;onpoid  p^rai 


•;aaj— tndep  p3}0  j, 


•;98j— mdap  no 


o 

I 
5- 

CO 

o 


•jaaj— atreid 
ratvpsp  aAoq^  aprnmy 


199J— I8A8I 

■Gas    Aopq   epnijjiv 


pa^j^nad  ssatupiqx 


188J— doj  o;  mdaa 


•V   (U     I      I      I    jj 

5  o©  c3  fl  « 

da  .5  <o  ^.2.2 


t^OlNOO 


OHONtO(Ot»OHrt!DM(CH»iOHN 
OCOOlOOCJCO'XrO-rCNOlHOlTfHTfO 

HOHOooHOioioiflTtiioooeiCH 


O    iO    oo 


t~  00  T  00 


COCO 


OOiOOOT-fMiOCli 

HOHrtOOrtOlli 


i  N  i!5  IS  00  M  M     OS 


>  <N  CO  CO     lO 


CO  CS        CO 


oaNOioinoM^t^H^i 

00C000O3CD(Mt^lMrtvCC0O-.    _ 

!>•  as  t—  00  00  OS  t-  oi  •^  -*i  -r  ■>»<  Tt<  00  OS  CO  -<r  00  Oi  00    t-    ->r  00 


<  (M  rt  (M 

•  ^3  T5  TJ  t3  ^  x 
o  o  o  o  o  g 

•  O  O  O  O   O  Ph 

.  :£££££&  iB 

'^OOOOOOC-^rt^^^rt^TJOcSr^'dOO 

u'O'tf'O'O'dfl'O.S-rt  <h  &  ii  -n  ^  o  h  -s  *d  'd 

«::::::  :*aww«po  :2  Wpq  :  : 


§*  i 

bfl       S5 

g   3 


i.O     o     >o       t~- 


n    oo    n    iflii      oo 
to    to    o    o  i>-      o> 


.H         CM      H      (N 


£         £         fc 


£     6 


o    o    o 


o    o    o    o  o 
fc  fc  jz;  fcfc 


O     O   O   O     C5 


tn     ra  oo  en  tn 

bf)    bX>  bX)  be  bX) 

bC     bXI  bx>  bCbJD 

■a  "c  "c  -c-e 

o  o  o  oo 


03    ■ 

Pi  • 


•rt  o 


3   ,d  ,3 
OOP 

CO      h      io 


O       O       O       O    O         r£) 

3  3  3  33    *fi 

O  O  O  OO     pq 


CSCN         '""' 


IB 


BLATCHLEY] 


TABLES  OF  WELL  DATA. 


529 


- 
J. 

IC 

c- 

s- 
a 

■r 

& 

DC 

-. 
~ 

X 

l- 

'  s- 

i 

— 
a 

a 

— 

0 

X 

s 

a 

s 

£ 

_  © 
CQ 

Z 
c 

0 

X 

c 

c 

- 

CD 

O 

"c3 
CO 

■  a 
|  c 

■i 

"o8*oi 

X.  X 

© 

"e3 

■3 

o 
o 

8  c 

c 

- 

O 
83 

X 

Salt  water,  905  feet 

Salt  water,  1,160  feet 

Saltwater,  1,325  feet 

Salt  water,  1,435  feet 

© 
© 

©    ' 

i ' 

CO 

O 
§1 

feO  o  tt  o 

52L1o§ 

CO  .          CO 

o 

00 

o 

■  00 
•CN 

■  to 

00 
CO 

1 

s 

~1 

o 

CO 

CO 

CO  00 
IO  iO 

iO  CO 
CD  O 
iO  CO 

o 

IO 

8 

CO 

CD 

CD 

»WMOOOM1«NOffl         <N  00  00  Tti  -*         05-*Tt<NrHCOCO'0(S03ai'*0)'*0 
O«00!DC»N"O^H05        CD  -*ti  iO  t^  CO        NiON^OONSCKMHHiOO 

HiHrtrtffiCOT-trHtO^M'W 
rtTl>COCO-*rHOOINHNCOffl 
(MrHOOTflCOi-HOOt-CO'f'^ICO 

MNNMOMOMOTf         OO  N  IN  !D  O         H(00?30)NNiOHHHOHtDO 
O^J'^^3r^NT)<^OalO         CO  IO  ^r*  CN  CO         N^NLOOONOM(OHOOOO>*0 
r-<  CN  CO  iO  00  03  O  00  CO  CO       00  O  tH  CO  >0        ONOiOOOiOHWfflMfflOOH 

~-  C.   D^  03  *— i  Tf  OS  O^  "^  CD  t^"  CD 

S    l-    r?  3L10CHMX1NOM 
(MMlCOrtMONOOOCi-l 

OiOWOOOOlNNH        O  CO  O  O  (N        iO  00  C  f  3D  O  N      ■  iO  iO  o  o  co      ■  o 
MMiONCOHNrtrtH        Tji        M^fH        XOHIN^iHlM      ■  CO  CD  ^  CN  CO      -CO 
<N                                    1-H                i-l                                                  rH 

.-H  IO  CN  i-s.  CO  iO  CO  -3<  CO        rH  IO 

OmiflOWiOI'MO')'        00NNOO        iOOOr~OiOiOOO-C;0>00<NcD 
C-NOOOMTfinoOOiH         CO'S'tOOOO         HIN^lOlOtlO'OOOOM'VlOinO 

OOOOIMC^i-OMtON 
-h  X  CO  n  t  -  C.  N  K'  OJ  CO  N  ■» 
0000i-n1cD00>-<CNC0iOiOcO 

c 
- 

a 
1 

•z 

'Z 

- 

4 

0 

c 

c 

c 

T 

p 

St 

1 

2 

c 
z 

5 

1 

p 
s 

4 

PC 

1 
) 
c 

c 

p 

a 

5 

EC 

c 
c 

1 

5 

1 
1 

pc 

3 

c 

-3 

PI 

Sp 

a.  - 

ZO 

I 

pc 

5 

s 

- 

- 

c 
c 

1 

J* 

c 

g 

c 
c 

1 

5 

',  -1- 

il 

.  a 

•  6 

t 

) 

c 
— 

p 

<r 
P 
« 

5 

- 

c 
c 

* 

c 
c 

c 

i 

b 
X 

PC 

1 

) 

c 
— 

c 

p 

a 

4 

i 
i 

c 
- 

9 

pqoc 

•t3 
•  o 

r-l         .      .      .  C 


o 

IO     .-H     00 

CO 

^      *-<  CNCO 

"-1 

OJ 

o 

o    o    o 

o 

o 

A 

fc  55  £ 

£ 

55  ^^J5 

X 

J5 

N 

S]       N       M 

s; 

n    c  c  c 

Si 

© 

fa 

>> 

o 

"o   'o   "o 

o 

*0     P<PhP< 

o 

0 

o    o 

o 

o  pqpqpq 

^H 

ft     P4 

ft 

g4  Pi  PI  PI 

bo   o  o  o 

T! 

-3  -3 

T3 

Si 

'C   'C 

Eh 

"S     S  S  3 

pq 

pq  pa 

po 

PQ    PQPQPQ 

330 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siajj^q— jonpoad  reprai 


•189j— mdap  p^oj, 


■J88J— Tndapuo 


•^88  j — airejd 
tnn^p  aAoq'B  eprvjpjv 


pa^aiauad  ssaujpnu. 


'183j— doj  oj  "qidaa 


02  .S  ©  ^.2,2 


•2   ~ 

$   - 

»fn 

^■s 

^* 

**s 

Ss 

342 

o  o. 

EH 

03  «3 

"o!  ts 


'  -^  00  CO        00  r-1  • 


Ot^MCOtDCONl 


'  CO  t-  <M  T 


MJOOHO 


i  o;  «!  •*  *  oi  o  t»  i<  o 

lOOooffiMiNmoi  ■* 


OMt^r^Tft-i 


•  r~  o?  oo  to 


_  C>5  OO  CO  (N  N>  IC> 

Hi-IOIC<3'fl''*ffl[.000)OH 


iO  iO  -*  CO  00   <*  U3  O  lO  i-O  lO  N  K3  O 


;ss°°sgg2^: 


iCiO        lOiOiO"— ICO        <tiiOO)C  OiOUJCQO 

LO00         I~~  ^J<  CO  CN)  c?>         C)  M  IN  O  "H  CD  Tf  t- N 
00O         <N  CO  lO  CO  lO         O  H  N  CO 'S"*  *  ©  H 


otoooioioei 


13  O         On   TO.W   O 

■flt)       T3  SO«t! 

pq  :     :w=  M  : 


o  o  2 

o  o  ft 

:p3  :  ippcoMWfQ 


;-abi 


oo° 
o  o  ft 

££§» . 

^^x)  o  o  o  o  o 

WMpq  :  :  :  :  : 


9  •  -a 

03      ■      •   O 
fl      ■      «   O 

o  o3  «.£ 


«2 


03"^ 
CO 


O 

6     * 
SB     g 

05         >» 


O 

s 

o- 


03  fi 


BLATCHLET] 


TABLES  OF  WELL  DATA. 


331 


©  CO 

"5.2 .2 
«2oo 
_«  •*-  to 


£££ 


(OHHrtOO 


TTOIOCRIN        <M        OO  rf  CM 

coo  oo  o< 


•  a    •  o 


fto 

CD    j> 

be  >* 


or 


CO 

g 

3 

Salt  water,  852  feet 

Coal,  760  feet  (lime  cap) . . 

Coal,  770  feet  (lime  cap) . . 
Salt  water,  1,400  feet 

c 
•m 

s- 

s 

•spjjBq— pnpoad  ibtjttii 

;      ; 

Is 

/5 

•199j— tftdap  i«jox 

CD 
<N 

o 

CO 

•j99j— q^dgp  no 

a 

03 
CO 

*^99j — guB^d 
ran^p  9AoqB  gpnixjiy 

VO  O 
HO) 

665 

1,109 
934 
774 
539 
329 

•^99J— I9A9] 

■B9S  Avopq     gpn^iv 

iO  O 
LOCO 

coo         • 

•  lO          HlOfflHiH 

•  CO       OICONCON 
00        CO  lO  t>  Oi  i-H 

•^99J— 

pg^j^gugd  ssgu^oiqj, 

o 

<N 

o 

O        1OO1OOO 
CO       (N^HCOCNiO 
•         i—l                      C<J 

•J99J— doj  oi  qidga; 

825 
1,000 

830 
1,110 

1,330 

900 
1,075 
1,235 
1,470 
1,680 

s 

c3 

o 
eS 

e     : 

o 

a  1 

"-1   ^ 

23       CQ 

:    s 

.     ft 

© 
03       "«        C 

33       PQ 

c 
X 

03     ■  o 

.  a  •  o 

■5*6 

O  C3^ 

:cqo3M 

Sur- 
face 
ele- 
va- 
tion— 
feet. 

o 

.           o~ 

O 

o 

o 

1 

c 
V 

0 

0 

0 

c 

•     * 

!   1 
!   J 

1  i 

3     5 

1 

i 

I" 
i 

3 

3 

c 

03 

1 

o 

'o 
*o 

I 

c 
C 

c 

C 

C 
« 

I 
c 

3              < 

>        c 

■5                   C 

3             < 

i 
3      c 

3             c 

3 

1             t 

3 

J 
i 

5 

0 

c 

1     ! 

3 

1 

a 
o   . 

23  o 

02 

o 

cN 

is 

IS 

CO 

CO 

? 

332 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


i 

to    • 

a  : 

3  : 
•c  • 

o  : 

a  : 

03     . 

^  ■ 
c3  : 

-d   • 

B  : 

3  • 
&  : 

; «  ; 

•«2  PI 

:    m 

.  io  p 

!      » 

'■St 

;-c3^ 

•  CO 

c 
f 

p 

r 
V 

a 

1 

- 
c- 

S  : 

^  ! 

3  : 
^  . 

.8    ; 

£ 

q 
o 

OS 

-a 

QQ 

CD 

o 

1 

o 
08 

? 

DO 

Salt    water,    1,850    feet. 

Well  abandoned 

Salt  water,  1,440  and  1,850 
feet.    Well  abandoned. 

sjaxreq — jonpoad  i^i^tui 

i 

en 

laaj— qidap  reioj, 

CM      ■ 
CM      • 

CO       • 

1 

OO 
00  >o 
»0  03 

io    •oc<) 

O        'OS  r-H 
t-        •  CO  CO 

O      -COCO 

cm     •  r-  oo 

t-      •OOJ 

•OS        iO 

:S    8 

•  r-T        Ccf 

•;aaj— mdep  no 

3 

CO  00  iO              CN  CO      ■  O  CO 
Tfi  lO  O               OO)      •  t>-  CO 
O  i-O  CO             CO  CO      •  CO  »0 

•03 

a 

03 
CQ 

•^aaj— au^id 
raniBp  8Aoqi3  apn^jy 

tO  lO  CO  N  M         i— I  .— 1  CO  CO      CO                   000>C0rt0>'WMMHO)NNON         lO 
tONO^O        j-jrtt-r-lT-l                 OOOffiHOOCHOCMfflOON        CO 
CO  CO  CO  CO  •*        O^COO     *S»                  CO  <M  ■*  CM  tt  OS  tp  CO  O  CO  O  CO  CM  i-H        tp 

laaj— taAai 
■eas    Atojeq    apnmjy 

wnoiocd      oo  oo  cm  oo    oo            otcoaooooooiKHOeqNN      co 

i-H  tH  i-I  .-I  O           ^OH-fll       O                       HNOINOlOOHTrrtTfHNM          O 

199J— 

pa^-i^auad  ssaujpiqj, 

O  O  O  O  CO        00  CM  00  CO     CO                 MOO00O 
T-HrtCMi-liO        rtCO        th     I-                 NrtlNININ 

t-co      • 

^o1M 

•^aaj— do;  o;  mdaa 

i-lNlOHIN         fCOINt-      ©s                   •f  CO  lO  O  CC   X   1  "   3  1  ~  1  -  IC  O  I-  O         O 

r-  i— 1  tt  OS  -fl*         CO  CO  f-  CO      T                   l005i01>CCNtOt^CDOO'*rtO)«5         rf< 
iflcOiOiOU)        QiOiOO)     lO                  tOtf)iO«OiOO>iOCO05iOa><OtO00        iO 

© 

B 

03 
ft 

s 

0 

> 

3 

■d-i' 
o  o 

o  o 

22' 

N  1- 

c   z 
c  c 
5  is 

it 

2u 

1 
P 
ffi 
b 

4 
| 

i 

5 

i 

p 

b 

1 

H         S 

E 

02 

o 

•8 

3e 

•T5  ^t3 
•  o  o  o 

>>  fe.   0)   fe   > 

o3  «h  — i  s-  a 

g  o  2  O     ■  S>       C 

fto  ao  .'-s     c 

Sur- 
face 
ele- 
va- 
tion— 
feet. 

or-      oo    w 

CO      CO         CO      Tf 

w 

CN           CD     CN        t~-             >0 
i^          t^     oo       r-             t- 

U3 

CO                      tO     1Q 

I 

e 
c 

a 

P 
a 
tu 

p 

c 

Sz 

s- 
c 

a 

1    b 

p 

5      c 

;    £ 

r    t. 

a 

c 

>         <B 
0        bi 

p 

C 

fc. 

0. 

c 

p 

c 
b 
P 

c 

a 

[a 

P 

a 

P 
3 

c 

i 

p 

J      t 

p 
2 

CO 

c 
a 

p 
a 

1      s 

(2 

O 

a 

)                tut 
P 

00 

o 
a 

P 
Ej 

P 
2 

-     o> 
6 

a 
P 

CO 
O 

P 
P 
CD 

d 

© 

o 

5? 

p 
s 
p 

d 

c 

p 
pq 

d 

o 
p 

03 
P 
03 

o 
pj 

PQ 
d 

>> 

I 

'o 

"8 

I 

o! 

M 
o3 

03 

03 

^ 

3 

^ 

d 

O 

bX 

2 

<D 

"5 
<» 
o 

O 

O 

bJC 

C 

c 
a 

<D 

(- 

"S 

O 

d 
O 
W 

Pi 

'3 
© 

o 
O 

p 

s 

< 

i 

a 
o 

p 

<^ 

"53 

o 

P 

ft  • 

03  O 

i-ifNcoi-i          cn      co            •■*               >o    co      r-        oo    os      o          ^h 

QQ 

1* 

BLATCHLEY] 


TABLES  OF  WELL  DATA. 


333 


©  © 
©-S 


©   ©   03  "^  >> 

©   ©   ©  Tfi    (3 

10000     .  ~ 


/d  ©    -.   ~   -<r"  en  © 

,og  03  03  eS^Vjg 
e3o>£££-'£S 

•S.<^03c3c3l50^ 


♦J  c 


t-  o  o  o  o  o 

edd  ddd 


co  CC 


88 


23 


O  O  ffll^  MO  «       cooooococooooocooo 


iNIMNM 


'  CC        Ci  00  CO  rf  CO 


HONHClTNfflflilOHNoiN: 


CC        OOHCOMiON        NNNNNNNNN         rt  00  OO  CO  N 


~  -t  x  r.^c^-TwioosXi-iooN 
~cocpco-g-CT>t'-ir~l^or-es> 


CrsOCCNCCOCNOOMNMiOM 
COHNlHtCrHNMlHCO  HIMrtNl 


O  O  O  O  O  <M  <J> 

io  so  os  ct>  co  cd  t> 


r-  as  co  »o  t--  t—  cji  co  co      o  >— i  co  *o  co 


O  CO 
t^  lO 
O  CO 


P  ©  bfi    .  J3  Is  © 


o   !  c3  o   • : 

ft  .  d  o    ■-*  ftd  o 

•fi-d  §13  go'C  §.d 
pq   ipaWcH^pamM 


Qdd 
03  o  O 

d  o  o 
'C  H  d-d.d 


WPh 


:s 


;^drd  b 


T)    t.    t<    1-        ■    S-l 

o  o  o  o    .  o 

>.  ©  ©  ©  £  © 

.  p*  b£  be  b£,2  bo    . 

O -t* d dd r3 d  O 


:pqcqco  :MpQpawo2PQ 


tj<  u0  lO  lO  - 


t>-      CO  CO  <N  ->3i  LO  i-l 

6    ododdo 


d    d  d  d  d  d  d 

i   r— r—  j-  r— r—  '— 


0000 
£  £  £  2; 
,d  ^"  ,d~  ,a 

Bl        lO        Ol        Ol 

■c  -c  b  "2 


d 

d 

o       ,d       ,d 
OOP 

O*  —<  CN 


«  £2  £2  S  23  £2  £2 

©  ©  ©  ©  ©  ©  o 

5  ^^^^^^ 

2  c3  c3  c3  c3  c3  c3 

a  sassas 

d  d  d  d  d  d  d 

d  d  d  d  d  d.  d 

c3  o3  03  o3  03  c3  c3 

©  ©©©©©© 

Id  fa  EC  id  52  Sd  Ed 

c3  c3  c3  c3  c3  ^  c3 

^  ^^^l^^rd 

m  mmmwmm 

1-1  CN  CO  T  IT)  cc  r^ 


OT       OT       go       OT 
©       ©       ®       © 


3 

d 

,?:     3 

T3 

73 

-d 

-d  ^ 

0 

0 

2    0 

Ph 

PM 

Ph 

Ph  Pm 

T3 

»d 

T! 

•d  t3 

& 

c3 

c3 

C3 

03     03 

8     N 

O 

O 

d 

Cfi 

<J 

3 

< 

<J    •< 

334 


OIL  FIELDS  OF  CEAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


cp 

s 

o 

c 

I 

.§. 

.5 

eg 
S 

s 

g 

© 

CO 

I 

s 

c 

& 

<D 

o 
8 

<^> 

§ 


•spxreq— ^cmpcud  r^ini 


laaj— q;dap  p^oj, 


•}88j— tftdep  no 


ranjep  QAoqe  aprimiv 


•JOaj— I8A81 


pa^BJiauad  ssau^opqj, 


188j— do;  o;  mdQa 


cm .2  »  >.2. 


GO 


_J?tv     ~_TCi> 


;oo«S«X<£5 


^£~£es^< 


co ffiOtcmOOOO 


ooi«c 


©to  o  o 

3  re  OS  r^ 

0  0)Oi05 


03  03 


H  Nt-^< 


i-O  <N  .-H 
00  t^  CO 


-2-S© 

03  03  iO 


©«•-«« 

COOm 

-r^os 

i-tOSOS 


'OO 


OOiO 
CO  OS  OS 


OOMM(N3«OCCtOt^vtOMOO( 

vot.'tfOOoonooTtiOfO' 


LO^COCOt^OlCO-^OCO'*! 


oooo< 


i|>0-*TTi-^TTi^lTj<-qiO-^0-^'0        •<S<Tri-q'-*ilOCX)OT}il^.( 


ONNlOi 


©  oo  oo  ©  o  o  to  as  i 


■  CM.  ©  IC  00  t~-  ©  ©  ©         ©  © 


.  _  o  rji  ©  o  cc-  ©  o> 

asosos©©coio©coioa5as 


\>&  fe  3-3' 


o  ft  a 


pq     pq^ccpq 


6  ft    . 

£&  : 

^-3  o 

^po  : 


o  2    •  o  o  o  2  o 
oft   •  o  ft  o  ft  o 

^  -3  .3  -c  3.3  -n .3. -c  -3 
:  :wpq  :mpqM«M 


O     .  c3  o  2  <«  O 
ft    •  fl  O  ftfl  o 

■3  o  otJ  o-g^'O'g^' 
'C  ^  ^  'C  ^  S-h"C  3*h" 

pq    :   :pq    :pq^pqpqWp 


©  — < 


t-     ©     <M     (M 

O     rf     O     iO 


re 


00 


oo  CO 
3  io 


N     N     O! 

o    6    6    6 
ZZZ,  £   £   £ 


P  3  3  3  3 

c3  c3  03  o3  c3 

3  CCfl  R 

c3  c3  c3  c3  c3 

,3  ,3,3,3  ,3 

o  o  t>  o  o 

2  3  3  3  3 

pq  pqpqpq  pq 


03  c3 

P  P 

03  e3 

,3  ,3 


00  rtTT  rH 

d  6  d 


J     jjj   J   j   J     J     .-q 


- 


3  3  3 

POP 

,3  3,3 

O    O   CJ 

3  3  3 

pqpqpq 

J  J  uj 


o  o 

££ 

sfef 

03  03 

P  P 

a  o3 

,3 -a 

CJ  o 

pp 
pqpq 

h4h? 


§ 

Q 

OOO 

C 

5 

C 

O 

AAA 
OOO 

^3 
O 

o 

OO 

-< 

rH 

o  ©  t- 

X 

33 

3 
01 

N 

CO  **  iffl 
CM  C^l  <N 

to 

CN 

00  OS 
CNCN 

BLATCHLEY] 


TABLES  OF  WELL  DATA. 


335 


S3 
£-2 


CO  © 


©«2.2 


OOO 


^O 


CD  CD 

10  o 

CO  CM 
.,     -«2   CD   CD  CD   CD 

*  g  "ioj  oo  oo  ic 

^£J   CO*  to   c/T  C/T  CO* 

^    ^    C3    Cj    Cj    Cj    d 

tcmOOOOO 


I  _|  INHH 


oo 

CO  o 


lOOlOH 
IONOOO 
lOfflOJO 


'  CO  »»<  CO  lO 


t>  CO  CC  CO  N  CO  O  IT) 


oo     -o»o 


tji  io  0>  i-i  00  ' 


Ot»<#OOWOT)ifqoOOcoOO 


"OONtoiotOMOoomo^Noooo 

COO)iO-*t<INiO00fOTl<cOiOC0ffltO 


iOMHlOO5iOTt"«HHCqN00H(OO)HrtN(DlOHO>Na<NN 
lO^OlNlOtMOCONOlNNCOOttnOWOrHlONtOCJOOONOO 

o-*tiTj<Tf!TfiTri-<fCT*<»-i',3,T*lcocoTt|eNio>o 


**it>.t>.Ottfil>r~-'Jt< 


WNho      •  lO  »C  CM  CM  CM -tfi  Oi      ■  00  <N  O 
-Ji        <Ni-l      •  tp  rft  CM  -»t  CO  Tf  CM      KMCOCO 


)  1>  1*5     i     .  io 


iooMOOnOMi)OMffl;?i  r. 

NOffilOtDfNOliO'ar-O-fNtO 

05co"OOi05coa5iot^050505'-oo>o 


'.".OXSOv     _ 

©COOOONCpO(N«    x   S  X   x  i-/oiooio^ftomooNM     _ 

oic^coioo5cNcoo5ioa>coiooic7>oa3  0~-05CT!coo5C7500ooor^o--a5 


-d.d 


cSg-gS 
ft  d  O  ft 


O^ 
fe  fto  £  ft 


l& 


^o^^oo^-go 


5    :S 

ftfe  ft 

sja 
;2rt2 

!  *-«,d  "-1 


d  T3  "£     .'  d  Th  d  "5  £  d  •=: 
d  o  ft  •  d  ft o  ftd  o  ft 

|>  CD      •  cS'<D  |>  CD  C3  t>  CD 
>5,bZ)t>^r*|ClX)>:*6£l^-(!stJ 


w .y  w>  •   .   .   . 

t)  o  o  o  o  o  orix)  o  o  o  o 

:&pa  :  :  :  : 


*& 


p  lO     1^-     h-iOiONCKN^Ol 


G>  C>  O  ©  O 


OOOrtM^N     CO     f^ 

rH  H  W  C>  Ct>  rH  Oi      C>      00 

lO  «0  lO  ■*  "tfi  lO  ■*     'J1     •'I1 


l  CO  CO 
p  t-  O0 


o       ,_, 

d 

55 


CO  >0  t-  00  CO  CM  -ft  . 


CM 


t~  00  i-l 


•  CM  LO  CO  ■ 


o  o 

15  !5 


o    oooooooooooooo 
fc  £55£:5£55:555£;555££55 


CO     CM     CM  CM 

d    d    do 
55  fc  ££ 


CD  CD 

MM 


MMMMMMMMMMMMMM    M    M  M  MM 


o  o  o  o 

fc  £££0000 

~  ^  ^^5555 

«T3  T3  'O  ^     .,.,.,., 

-d  "d  "d  73  ,>>,>>.>>>>> 

o  ooooooo 

Eh  E-!  Eh  Eh  CO  w  co  02 


CO 

Tfi 

CI 

>-lr-ICM 

o 

O 

o 

55 

£ 

55 

Z^Z 

fl 

a 

ri 

pT  d?  pT 
2  3  S 

C3 

a 

ect 

d 
crt 

§ 

9 

^SS 

,ri 

rt 

A 

-3,d,d 

o 

O  cj  o 

S 

d 

d 

a  d  d 

W 

pq 

pq 

pqpqpq 

w  w 

5= 

Waw 

o 

o 

o 

ooo 

_o  _o     _o_o   _o   _o  o  o  o  o  o  o  o  o  o  o  o  o  o      o 

_o o    oo  o  oooooooooooooo    Q 

O  i-l         MM     ■*      LOfflt^MOSOrHCNmtlCtOpNM         03 


o    o    o  o 

3  3  32 
o  o  oo 


.2.2  2.2.2  2  2   d   d 
2222222  o  o 

OOOOOOO   Q   Q 


d  d  d  d 

CD  CD   CD   CD 

bC  feCbX)  M 

<  «< 


d  d  d 
ooo 


336 


OIL  FIELDS  OF  CRAAVFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sjaixeq— lonpoad  re^ini 


'%99l— q^dap  ibjoj, 


•:paj— qjdap  no 


ran^p  9Aoq,e  oprumy 


•199}— ]8A8l 

■eas  Avojaq     eprupjv 


•189J— 

paiBj^auad  ssau^oiqj, 


■^9j— do;  o;  mdaa 


8  1,1 


C3  O 

S2 


-3 

a 

o 


^  o 


££ 


Ph      com 


<D  <D  <D  ,-. 


££<S.2«2fe 


r  = 

"   :■- 
r-  e'- 


er c3 


Oco 


« 


<n    •  ire  t^  o  o 
O     ■  r»  i^-  [- — r> 

O     '0)05  010 


t—    .1-nreco 


MOtONCOOOONffiOlOO'COlN 
lO00<ON        (OHOCONINoOHlNrtHOlOOlOiOTCcCHTHaOJlO 
f^fHTjt  -qi  T*l  Tfl  Tf  T)<  Tt<  ire  r-i  Tf  ,-|  CM  Ttl 


'CO       NTfHHN 


-'.      —^    '    .»   <— '  TP   (_J   UJ  <_;   "^T   ^T1    11J  U*J  ^^   L*J   L*J   ItJ   -rp    UN   I.N   C^J  t^J  (JJ   T"   >-*J  <JJ   ^T* 

tOO)C5!D        (£>OS05tOW*0'*'<»ln<'*0)0>05020)OMOi<Ot-0) 


O    ri 

ft  a 

pqpo 


^T5^^ 


b°  o  © 

■*  fto  ft 
55  ©  >  ® 


O  O  OT3  O   O  O  O  *_, 

,rJrd'd"Cd,d,d'd'd 


o  . 
ftfe 
ft  5 


o 

ft 


s  s 


i  io  >re       ■*< 


o  o 


as 

U.  it 

-d-d 

B  S3 

WW 


B  B 
<<5 


33 

o  o 

GO 


—     '-' 
c3     © 


o  o  o 

£  £  £ 

ft  ft  ft 

<S  <»  <x> 


o    °66666 

n  eftfffg~ffg 

.  *      ,  -,  ^  c3  ^  c3  « 
O      O  C3  c3  C3  03   C3 

o  o  o  o  o 

u"    J  S  3  3  3  S 


b  b  b    o  qhjkJvj^^ 


o    oooooo        o 

S  3  3    2  222 222     2 
£  £  3    o  oooooo     o 


r-c    cn    co 


co   i~  i-h  cn  co  ■*  ire 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


337 


5  «■ 

—  co 
o 


3       ^jj- 


— ■ — o  dq  a 


—I  CO 

OO 


~    -© 

S-.    U    Qi 

©  ©  *3 


OO  £  £:0 


GOO 


c3  03 


►  *! 


_©  o 


©d 
"o3  O 

>   © 

co£ 


l^  tt  O  lO  !N 


11 

to 


\~~  O  X  l^  n  n  t-  K  C  N  W       O  N  OC  -r 

r-ONNHX-lrt-II^Cfj  r-H   CM   -H   CM 

050©ffiOOOCOO)Oi       ooco 


<*      toco 


O  O  O     '  O     '  O  O  O       o  o  o  o 


0!!O       '  O  ~V 


CO  o 
O10O 


IONHU5N       -h  n  -^  «  /.  -.  •-  ?  c  ^  /.  n       x  to  o  o       I^»-J*C 
'^•??5?£J5?       S  ~  ',2  £  =  2.1  2?  t£  2T  IT  'S'  £?      ^3  :=*  £2  9£      2t;0( 


'CO  coo  OO 


000      0000      ocn^h— <o 


HrtlOrHiHOlONffi'<rX( 

hiOm«OhO!SU3»H! 


m  «  a  «  n  1-      o  to 


XM-HTT-OMN! 

■*  co  1^-  t^  tc  r-  to  10  ; 


S?S>oo  < 

■*  CNCOCO" 


=  = 


tO  O  -T  to  CO  CM  I  -  1-  CM  — 1  f  i-H  r-  CO  CO 

Oi.or^Xrt-rXXO-rCMO-*-*0 


cm  t^  t^ 


/^■OOOiH  1.0  lO  o 

co>3*-*-i^-w"Cmcococo 


hNNCKJC! 


SiO  00  •*»<  <*  t»        --OO 
HMOW         O  tO  CM  -P  CO  'O  I-  tO  t~  1^  CO  -W 

UJ!0«0>0)0        COOOOOOOOOOOO 


-r  x  o  o      o  1.0  o  t  o      o  o  0  o  m> 

O  X  X  CM         to  01  O  O  tO         O  i-O  OO—i 

0000      o  1^  o  x.  o      x  o  r~  o  o 


iCO-rOOOieMCfliNOnDLCO 

r.  t  v:  r.  /  ■?  modnhqnnoon 

xtoox-^totcoccoeocoeot-o 


>d  o  o 

I-CX5T5 

:cq  :  : 


o  .  . 
£  ft  .  . 
o  ©    •    • 

JM    •     • 
'CS'd  o  o 


O  c3d  03d        CO  c3"d  £ 

^  £ 'E  £ 'C      ^13  iz'C.Z 

IcofflcoCO         ■     'cOfC  J 


O 
ft»c  ft 


=  *e 


>"C  c 

l-C-0 


.coC£coccP3 


£-  OlKiCO 


coo    o    ^ 


c 

■sg 

.§« 

co  i-3 


tCi-O 

6  6 


o  o 


c  c 


03   C3 

c  0 


o    ZZoZo'ci 

rn    ,C  A  re  ,fl  ro  el  rC  rC  r£  ro 


ZZ^Z      g    g 

c?c3g  g       «     « 
coco<J<!     >   > 


c  o 


•fi-E 

CN 

^  6   " 

0 

03  C3 

O 

c^;    0 

j?| 

b  fa 

y 

fc*.  z 

XJT3 

tn 

is. 
ray 

is, 

ea 

S3 


^c  ^  o 


22 

CO 

:22s 

©  © 

© 

•  ©  © 

3  3 

:  a  s 

to 

TJ-O 

-d 

■  d-d 

s 

OS 

p  O 

0 

Sh 
ft 

:22 
:ftft 

I 

1 

8 
— 

g 

"d-d 

T3 

:tw 

- 

W 

P3 

P3 

*) 

©  © 

© 

•  ®  -S 

p 

S3 

fl 

C 

c 

c 

c 

11  08  c 

d'l'lc 

"  * 

b 

K 

« 

SI    N 

ft 

?! 

t% 

ft 

© 

£ 

5-= 

J= 

w  "S  3£ 

SSS22 

2  2  §  « 

h 

C 

3 

ll 

feJ; 

s 

C0)J 

CO    J 

c 

CO 

0 

SC 

C 

-s1<1C 

<-c 

0«<<!OC 

OOJh3 

^ 

- 

J 

j; 

cc 

C 

t^ 

000 

0 

-HNCO-J1! 

to  t^-  x  0  0 

,- 

•- 

0 

^  CM 

CO        Tf 

,_! 

,_ 

22  G 


338 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siajxBq— pnpcud  im^ui 


"IQQi— q^dap  jbjo  j, 


•}99j— qidap  no 


•}89;— I8A8{ 

B9S  Avopq     oprnmv 


•J98J— 

pa^jjonad  ssatnpTiiiL 


'laaj— doi  01  mdacr 


3  s.2  p3  a  « 


a)  jj  ■  a>  o> 

<x>;=.  "as  <u 

*->  c3  '  *"  '— ' 

co  ,  co  cs 

«o  ^  .  co  »o  . 

fH    O  •  fH  1-1 


+500. 
c3  *C 


0)<N 

CjlO 


toO     co     coO 


<D  "S 


•Slllsll 


c»    oooo    o 


>-io 

p 


(N»t-CO 
CO  >0  lO  CO 


ONON 


CM  OS  CM  ONOON  tpiO 
T»<  -»3<  fH  lo  lq  -FP  t—  COCO 
CO  lO  CO       iCiO^OiO       io»o 


(-1  — 

flfi 


sgs 

t^oo 


-£ 


™p 


CCOMtH        fH        lOrtMcO        OOH00        t^cOCT>FHO>fO>COIM<M 

^■ocof      t—      r-i-coco      cocooon      t^  co  co  oo  >o  cm  co  t--  cm  co 
co  co  co  co  co      eo      co  eo  eo  eo      co  co  eo  co      cocccoF-icoocoeococo 


CO  CO        I-  i— i  t—  CO  < 


I  CM  CO  CO         -*  rt< 


CO-*fHO5f-icOf-I1^0000 

CMcocOF-i->cfr~coCMt-~co 


O  O        -f  Oi  02 


OO         t^OOOf  00         i-(         t-  »■    /:  M 
OlO         KJfTfON         "CH         CO  CC  -r  VO 


ION        lO  lO  lO  CO  lO 


lO  lO  CO  CO 

mioioio 


LOfflNwcoio 


I, 


F* 

rM    O    O 

•  P-p-P 

W  :  : 


<?-p 

-O  o 
°  8 

O  te 


WW 


-^  o  ftfl  o 

:  :  :^MfQpQW 


o  o 
o  o 

•a -a 

312 


sss; 


>0  CO     CO     Tf< 


•^    o 

•s  * 


cni-c-Jco  o 

-  -FT  ~«5 
s  2  «  S  to 
p  p  sh  p  cu 


CO  CM 

d  d  co  -*> 

HH    O    6 
P"  PF?   Z 

aa^ 

XM  P  P 


to 

p 

o  o'p  o  o      o 

3  3  §  3  3    3 

OOhOO      O 


HOOO 

dfcfcjz; 

£  p"  P~  P~ 

£aaa 

P  ,*,*,* 

,q  o  o  o 


O  O 

CM  CO     £h  f5 

^     S  fP 

g   pT     tC  60 

c3  a  '53  'S 


oocc  2222  22  2  2  .2 
S2SS  3332  33 3 3  3 
oooo    oooo    oo  o  o     o 


<M  CO  -Cf  rH 


iC  CO  I-  00        fH  CM     CO     •f 


SZ 


•T3  o 


t^     W     W 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


339 


^   -2,2 

CO  ti  "S^ 
O       CO 


C5> 


3S 

C3<N 

coO 


jlil 

sgsg 


aj  05  05  .05  . 


<M  co  r~  oo.; 


■*»  in 


05  0)  ©  05  05 
-~S  .ps  +j  -»J +J 
c3  C3  C3  C3  c3 
£££££ 


d  s-< 
C3  iS 

>+3- 


'Qfi 


NOOWH 
CO  »0  >0  i-H 


:83 


loaooCLOtsoooOM      co  oc  co 


lOiflinoovgi 

lOWTOt^HN 
>  t>-  CO  CM  IN        Oi  CO 


lOtOV^fflNOOOHiOrtONOVOOOOh-        TNh.        OOlOiOOC 

oo  co  io  co  io  •*  lo  io  co  c~  as  t-~  to  oc  ~  r-  :c  —  eo  o  co      c-.om      no^wom 
•*  -*>  io  i>  c~  ■*  c<«  ■<*!  ■*  •*  o  io  oo  i-i  (M  co  lo  oo  i-H  oo  co      ttor-      ^oohnw* 


Oi  O        O0        iO 

TJ1  Tti  LO  CO 

1— t  CM  H  i-H 


csr- cm 

co  ^r  >o 

IN  CO  -31 


COCOCO         i-H  ■*  i-H  T  CO  <N  -qi         i-l  i-l  i 


NNiOflNOO^KtOOHONiOijOOOOl 
■^lONONOOrtNMtDHONnNOOCOirl 
OJO)OMlNail>©0)OiOO?5Cl>t^O<MONI 


MOO        OOUJUJOOiOO 


88 

■oo 


0373  O 

com  : 


-3  jh  C-O 

o  o  cs  o  •  r; 

bO    .     .  >»    .  6j0  >>  tJO    •     .!>cjo2?050 

'doOdO'dd'dooW'0^03 
pa    !    '.cc    !  pa  co  PQ 


T3      '   L>> 

■ass 


'.WmmWEHSmpqW^S 


T3  O  h 

pq  :&q 


pqpo 


tS  c5^ 


05   ►> 

tu)R 


Pa« 


o  o 


**0      . 

•    •  o 

O  0>7 

££~ 

CJD  fcXT3 
'5 '3  C3 
WWW 


c  o  o  o    • 

fc  £  SSI 

s  £  flpl  r 

C3'    03  c3  a  .2 

d  fl  flfip, 

c3  c3  c3   c3  cr. 

.a.  ,G  A^v 

o  o  o  o  — 

pq  pq  pqpq^ 

<5  -si  «i<i^ 


o      o 

3    3 
o    o 


IS    I 

,d,d     & 
mm     co 


K** 


«     c3     c3  03  c3  rf 

CO     CO     COCOCO  CO 


ILO  rt 


I*  1^ 


1* 


340 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


•siaxiBq— jonpoid  p3i}iui 


•:}98j— q^dop  ibjoj, 


•?aa;— qjdap  no 


•^88j— aire  id 
ran?ep  aAoqB  apnii^iv 


138S    Auqaq    apn^uv 


•}8aj— 

pa^BHanad  ssau^oiqx 


•;aaj— do?  o?  q?d8Q 


co«2  «>  >.2£ 


S£ 


SS5*  o 

HOH+J 


££•5 


S  30 


Offl 
to  CO 


-r  O 
<N  O 
COCO 


(NIC 


(_,•     ooieooo 

q        NrtMTNM 


IO  N  00  O  Tf  Ol 
IN  CO  lO  "O  ■>*  lO 
CO  CO  CO  CO  CO  CO 


^  O  O  00  CO  CO 
»H  CM  »H  -H  CO  CO 


CO  CO  CO  CO  CO  I 


cooiocccOrtior^ONOcoNrtoiwoomffiooiomoooO'* 
NiOTticooffltoociofOoctooiiifiNoioainHioow 

CO^hOiO-*COCOCOOiO-«j<COCOCOCOOiOCO-^<>-h05COCOCOt-i 

O)  O)  t^  ffl  O  IN 

KJOI^tOlOlO 
co  to  CO  CO  CO  CO 

1^  O  LO  tt  IN  OJ  'O  M  O  X  O  N  X  O!  H  N  (N  N  H  O)  1C  N  N  CM  (O 

IN-»iOt005WMiHiOiOOrtCCOiOiONO»0'<f«*(»!0 

>-Hco-*a>o^^H.-iTt'a}^H^ao^Hi-iT*<cs^oco»ooo^H.-ico 

■*  co  oj  co  in  -*»• 
oo  oo  oo  oo  oo  oo 

UJHHM 


OilNCO(NOCO(NOOOOOOI^>OcOi 


lO  O  CO  "O  O  O  tp 


CO  CO  CO  CO  CO  CO 


wspScoS 


o    •  2  o 
o    ■  d  o 

:  :  :coccW  :coM 


O  03  o  o  r? 

o   •   • Ad o  o# 
•^.S'O^'C  3 -d-d  o 


CTJCN  CO 
l~  00  X1 


CN         MNi 

6 


o  o  o  o  o 

*0  'O  '&  r0  *0 

5)  0)  q  ©  C? 

0}  O  C5  05  © 

cocoa)  w  xn 


in     cocoa)     a)     co 


o      c 


o  o  o  o  o 

£££££"-: 

d~  d"  ef  d*  dS 

c3  CO  c3   C3  CS^"1 

d  d  d  d  d_r 

C3  C«  c3  C3  03^ 
,d,d,d,d,d  g 
O   O   CJ   O   Or/) 

d  d  d  d  dra 
pqpqpqpqpq  g 


d 
o 

C/3 

1 

U.     (_.    fc. 

d  d  d 
o  o  o 

S 

C3 

,d 

CO 

g  p* 


-d     ,d 

CO       CO 

C5  O 


lai 


2  2  2  2  2  2 
3'.332'.33 

oooooo 


Ifc 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


341 


- 
J 

50 
M 
EC 

r 

C5 

<2    .'    .' 
o     '     • 
°    !    1 

<-H    CO        '• 

-«2   ; 
o  ■<*<   • 
*%   ■' 
►-?  : 

^  v-      • 

■j- 
C3 

CD 

S3 

o 

s 

.a 

CJ 

CD 
<D 

CO 

co_^ 

s 

c5 
P* 

"c3 
DQ 

c 

5 
- 

E 
0 

"a 

3 

e 

c 
- 

5 

- 

OS 

"a 

I 

g 

s 

o 

c 

c 

M 

O 
-: 

c 

OlflOCOOOOO 

o  ■-  :  :  !■;  n  2  ;  m 

'"-ri^rtN 

CNCNCSCCMCNCNCOCM 

L-0 

CN 

^S 

o 

•  -. 

•  0 

DQ 

CN  CM  O  l~  C-}  X  X  l^  CO 

'O  X  —  CO  CO  CO  O  CO  r- 

cococococococococo 

~  3  32  "*  M  '- 

CO  lo  CO  CO  O  CO  CO  CO  1  - 

o  co  80  t>  CO  O  00  t~  -o 
cococococo-~rcococo 

C-l  X 

COCO 

CO    c  o 

ri 

CO 

CO 

o  >-o  o 

CO  CO  CO 

—  t- 

coco 

BO  lO  CO  i-I  •* 

■J  M  M  M  M 

•o>o  o 

co  co  T 
rococo 

LT»       'HMO 
-h  Si      iMfM 
CD  CM      'M?5M 

O     ■  O  «0  i-h 

CO      i  -r  lo  t- 
00      •  CO  CO  CO 

-H  X  l~ 

t^  CD  LO 

CO  CO  CO 

co  o 

o  t- 

CO  CO 

CO  CO  DO  OS 

CO  CO  CO  CO 

CO 

r~-aoo 

LOX  O 

§ 

•a 

ro 

5 

I- 

i 

5! 

■- 

M 

i- 

■  o 

co 

- 

t^— i  CM 

i  -  1  -  CO 

— 

x  cm  cm 

—  co  — 

§ 

o  -o 

-  - 

IS 

2 

>0  co  cm  lo  co  t>-  CO 

'-0  lO  —  co  —  —  c 

CO     C"} 
lo     ^r 

s 

5 

wcoujc 

oo^ 

i- 

C_ 

2 

-3  ° 

cococococococococococococococococovococo       cocococococococococococo—     co     co  co  co  co  co  co  • 


fioNH»f[,3xz  r-  co  ia  co  as  x  -o  cn  ae  x  — i  ©  -r  o-.  o  w  —  ■-  r-  x  «  —  co  -r    ih    x  —  t — ioooiohi-in  •-  x 

co  cm  CM  lo  lo  co  — i  co  ~r  ~r  —  ■-  —  —  oi  co  o  >.o  co  x  co lo  lo  i- •/.  c  u-  l»  c     —     '-  <o  i~  ■-  co  lo  co  uo  lo  —  —  lo 

X   X   X  — <  X   X  X   X,  X   X  X   X  X  —i  X  X   X  X  X  X  -r  X  X  X   X  X   X  X  X  X  -*  X  00  CO      X      X  T  X  X  i-h  —I  X  X  X  X  X   X 


^x! 

O  co  c 


X  CN  O  TT  -H  O  t^  CO  CO  CO  O  CO  CS|  CO  CO  -r  —  CO  —  CO  CO  O-  I  -  i.O  i~   —   —  CO  — ■  i-0  C-l  lO  CO  CO      t-      X  CO  CO  CO  CO  C  CO  t^  O  UO  LO  < 

—  -H  H  CO  CO  —  — '  CO  -r>  CO  CO  CO  — '  — ■  OC  — '  CO  CM  — '  X   —.  — <  ~J   CO   -O   X  r  -  CO   i0  I  -  OC  t  -  I  -  CO      CO      t-  I-  I-  CM  CM  —  CO  CN  CO  H  CO  < 
COCOCOCOCOCOCOCOCOCOCOCOCOCOcCMcOCOCOCOCOXCOCOCOCOCOCOCOCOCOlOCOCOX      CO     co~cococococococococo< 


r-)  lo  c 

O  X  t> 

~  X  lO 


c  i  c'^f  c  c  :'  c  d  d  d  d^  d  c  d  d  o'q  o  i  c 


ioooo^^^S 


Sti^tooooo     -S  *°  -S 


SSS     gg 


X— iCOOOJCNCOCO     t-     -h-cOlOTCO     C5     S5 


CO     tOI-t-t>[>     CO 


OS  CO  CO  LO  lO  C5  -J  t^ 
l-XX-CN-NC 


COLOcOCftXCOtN        COCO 


ccn  cr<i  c<i  co  ■ 


coo 


oooooooo    o 


o  o  o  o 


o  c  o 


oo  o  oooooooo  o  oooo^ 
oo  o  oooooooo  o  ooooZ 

cs    c    scdgss^ffd    S3    g  Q  g  g  "3 


c    o  c  o  c  c  c 


z  zzzzzz 


o'  c    d   Z 


o    c 

z  z 


:zz  Z   B^g  f 

"--MS        N ^«        O 


'II  'X  rx  CO  CO  CO  J  ij.    J     OK 


o  c  dddddddoo  o"~«To~ 

Z  Z  ZZZZZZZZZ  p/S/E. 

"d  -o  ■onj-dtf tTi3 rf'O'cf  J^_2 

o  O  OOOOOOOOO '  — 

O  O  OOOOOOOOO  — ■•- '■- < 

CQ  CQ  COCCXCCCCCOCOCOO;  OOO 

si  ffi  ^' jj jj J^JJ  <<< 


oc  o  ooooo-o_oo_o  cogoc  o  cocoococ  o  oc  o 

22  2  S22S22SS  !2  33332  2  22222222  2  22  2 

OO  O  OOOOOOOO  0  OOOOO  C  OOOOOOOO  Q  CO  O 

t-  X  CC  O  —i  CM  CO  T  LO  CO  t^     X  C">  ~  —  C\)  -h  c>}  CO  T  lO  CO  t^  X  0~.  O  pH  h  CN  CO 


•  oooocooco  :  :  : 

d    d  ^  —  —  —  —  —  ^- fe  ^  odd 

■g    "3  M  M  cj:  cx  cx  M  cx  u  bye  222 

5  o  S IS S r S jE '£ S 2  ooc 

<*     lo  wi  CM  CO  ^c-  lo  co  t-  X  Ci  hh  CM  CO 


C^  CM  -M 


Iz 


342 


OIL  FIELDS  OF  CRAWFORD  AXD  LAWRENCE  COUNTIES,    [bull.  no.  22 


03  o3  +i 

b. ,    03 

©  > 


o 
u 

I 

,gi 

CO 

S 

O 

si 

o 

--c 
•<& 
8 

to 

! 

$ 

O 

to 

o 

to 


CO  lO  t?LO  t-  CM  i-4  <©  Tt<  O  iO 


•spiieq— pnpoad  WW1! 


•}88J— q^dsp  I^JOJ, 


iO(005COM(0(OtO!OM 


'590J— qjdep  no 


CM  O  'OlOWiOOOOOlH 
t^O  •  Oi  00  CT>  C7>  i— I  t^  C7>  CO 
lO  CO      -iOajCNliO«5lOiJ0CO 


•198J — 8UBld 

xnn^p  OAoqB  epnipiy 


iCDCO>OOSiH' 


CO  o 
o  o 
CO  co 


■B8S    A\oiaq    9prniiiv 


i 


O  X  *  'V  i-l  H  N  UJ  rt  o>  !0 
OCOMNOlOCONIN'VlO 
HrtHOinMHHHHOO 


CMO 

CO^f 
H00 


•}88J— 


NTfOOOlONffl       •  CM  CO  OS 
CM  CM  il  m  i-i  CM  -<J<      ;C0i-HiO 


•;98J— do%  01  mdd<j 


cc  o 

I-  00 
■  O  CM 


OOONOCOOOiOlOOHO^OlNfflNO 
tOlOtOlOffliniONNtCONNMlOCeO 
MOC<5COCDC050COCOe<3CCMO>!OMTP'0. 


NXi-l^NiClOOOOtDrHM^MO 

co-^coT*co-*«>*'<Mcocoi-icvi<McOTr'^HO 

X  »-H  lO  00  r-i  O  i-H 


lOOOOOOOOi 


r-OOOCJOOit^t^oi^oc— <cOTfCM-H 

lOMCKNCOWiClOCNlOOMOlOO 


i3  Ct5  fl 

O  *  O  03 

O  a  O  pa 

£  03  £  03 


s-g 

S  o 

03£ 


:pqM 


cawM 


rzi<5  ©  >.2< 


O  <-H  CM  CO  00  00  f  CO      lO      CCO      -H 


dtCCCWN^O) 

iH  X  ^  lC  lO  ^  ^  CO  'fl'TfTt-Tf^OOCO^O 


U0      CO      C>      O 


03-^ 

O 


l-O  CO  .-ICC 


co  i-i  r~  co  io  cm 


OOOOOOOOOOO        oo„_ 


-*  CM      CO     00 


.2*>2"'2~2~®2",2~(3^2'22>  arsf^^^^^^z  !z  !zz  *z  *z    ® 

05  05  ©  ©  ©  ©  ©  ©  ©  ©  ©  ©  ©  n^j  rr)  »rt  rrj  rrj  rr)  "O    "O    'O  T3    *C    "C     fl 

^^=3=3^==^^^=:^  =2^©©«©©©g     g     gg     05     ©     © 

bSSSSSSSSSo  bbiMDQffiiaffiffi";  «  ^m  «  m  "S 


§  . 

•rt  o 

©^ 


OOOOOOOOOOO 


O  O  O  o  o  o 

0  p  pq  ^  pM  pM  pR  pt( 
M  CJD  bJO  biD  bC  CJO 


ooooccoccoo    oopacncqpamcQO  o  oo  o  o  o 


o  o    o    o    o 

a  fii  53  3  3  3 


O  CC  l>-  00  i-l  CN  CO 


lho     N»ac 


L» 


r~  i-H    <N    co 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


343 


■r   -j- 

03  03 


c3_; 
3£ 


£fe 


O  10 


oo 


wo 
28 


ooioomio 


cm  i- 

■  -  ■- 
oo 


wmioio 


O00      -00CO 


O-H 

SO  ro 


re  —  re  - 
l-  lO  iO  i 


lO  UO 
lOuO 


•i-NI 


en  o  •<-  co 


M  O  r.  C  C)  N  M  N  N  O  ' 


•*omoc<:a.  M^-v^'v 


CMOCOTi-.^TjiCOCOCO'^'' 


OCMN»' 


lOOC  o 


Or-  -n 
f  r-  r- 

O  O  -a* 


toteno: 


XOHC'/rc/::/  C  •-■:  C  cc-^KicOl-o 
I  -  «  Z  ?)  I"!-  C  M  n  '/  ~  c  ^  u-  n  o  t^  m  h  cc 
OhttWCNCXCCOhhhOOOiOOOO 


ooiaion 


i  OS  io  o  o 


OOOHOrtOONNMMN 

toNioweowoiowo 


W  O  C!  H  N         O  CM  u-  t-         IC  lO  lO 


micco 


LO  c  o  n 


o  oc  o  ia  o  ic  r-  co  r-  cm 

Wr/CCCWCCN^TfaHWHtOOi 
NCONiOLOLClOiOiOiOiOlOffiMi 


03  o 
PI  o 
c3£ 


=  = 

Pi  C 


o  S  o  c  5    !  c  5  >?  2  2°^ 

•    •    •    -^-S^  g    .  t/c  --  .^  tr-  ?5 

-C  T3  TJ  T5  -r;  a  .H  "£  ■=■  "0  "£  •-  a  t=^o 

:  :  :  :cq    ^a  ^  :a^§  ~~^g 


o  o 
o  o 


Si2i2 


■^~  fa  S^  ■  fa  S* 

o  o  °  <3  o    ■  °  S  o 

O  O  PnP  O     •  ChT    " 


^^cc^J?:£^ 


^  o  c 


i(Nrt(N 


IT)  £  P^ 

>  o  P<p  o 


"D  T3  T3  "O 
O  O  O  O 
O  O  O  O 
££££ 


CT>     O  — '  O  O 


Ci    r-.    r-    r- 
cm    cm    cm    CM 


o    o 

fl  p? 

n 


o  o  o 


.     .  °.2  2 
6   o"g,ftg, 

H      H    t     •_     ii 


£  rs 


ooo    o 
eteen    EH 


c  d  c 

c3  03  c3 

>>>>  >-. 

cdo3  p3 


t-  CO  lO     CM 

6  6  6    6 


o    o 


^  •  g  fc 

£ 

^  ' 

£££   !? 

o     © 

o 

o    o     o      - 

Ci 

fc  £  M   « 

,.,       03 

03 

pi 

03 

PI  P  fl    pi 

7i  c5  r3     c3 

cS   s 

o 

Pi    Pi    2    ^ 

>> 

>. 

>>>>>>  >> 

C3     C3     °    03 
>>    >>    o      • 
03   03    w   O 

« 

« 

P303P3    03 

o  o 

O 

o 

o 

ooo  o 

Ei   ^ 

Ei 

^3    ^ 
O   O 


o      o    o  o  o  o 

o    o  oooo 


o      o 

2    2 


.2     .2 

2 


o    o    oo    o 


2  2  2  2 
o  o  £>  o 

14     CO    t^     00 


o        oooo      oo      o 

2      222  2    2  2    2 
o     ooo  oooo 


rtNM     -* 


\±± 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


1  <£«2 
o  >o 


I  03  OS 


is; 


_© 
o 

J 

S3 

■O 

CO 

Si 


•spjj^q— pnpojd  ibi^tui 


•}99j— q^dgp  i^jox 


O  to      •  CO  io  >o  iO 


198j— q^dapno 


IO  IO  IO  CO  IO  >o  lO 


tun^p  8AoqB  apn^i^V 


O  CO  •f  -f  Tt<  CO  tT  I 


O-^OcOtp  WO' 


•}99J— I9A9I 

B9S   Avojgq   gpn^t-^v 


199J— 

pg^j^angd  ssgn^OTqj, 


'199J— do;  o;  q;d9a 


5  O  »  o3  PI'S 

to  .2  ©  >.2,® 


SZ 


iOOI^hoih-/   C  :~ 
05  <M  CO  IQ  IO  C—  " 
--F  00  O  O  O  t 


oo  o  o  o 


NCOCOCOMOSNO 
■~  O  CO  CO  oo  c-. 
IOOOONC 


iOOt-(»OnO'*l-.'»^ffliO'1'i(!Oi,l-OOil50llvOOOOO!0*N 

in  io  O!  «  t  o  i-  a  i-  i-  a  n  H  c  w  c  oi  /■  c-Mi^OHoioaiMcooiHiH 

02<N'-J'iOtOCNiOCNiOa)i^iOO>OCOiO>ni,CS^a>CNiO'OTti05TfOSCNTfNiO 


O  03  o 

ftfl  o 
XI  d-~d 


d  2 
d  3 .2 

:cqM 


03    O 


s-  dx) 
O  o3  o 
ftd  o 
»e3  fe 


o  o  o 
o  o  o 


'ftOftflO 


fed  fe  dd  d"d 
fto  ftd  oSo 


-n  g.S'd.S.tS.fci'd'dTJ-JS'C  p  •-  d  d  -c  .d.  -c  §  .is  |=j.!h 


O        t^-H     (M 


00  00      CJ5         O      CO 

'fv     *        io     •**     ■* 


i- 

t^ 

0C 

a 

c 

CN 

-r 

IT 

X 

c 

ON 

S 

.' 

c 

c 

c 
5z 

c 
V 

c 

c 

c 

C 

c 
V 

c 
V 

c 
2 

C 

C 

c 

I? 

•c 

es        v 

2  2    2 
p/p,  p 

CO    CO        CO 


0$8»ffl0)©00) 
"ft     ft     ft     ft     ft     ft'ftft    'ft 

cb^C3CiCC5c5C)© 


OO  o 
t^fH   Eh 


O   O   O   O   O   OOO   O 
EhEhEhEhEhEhEhEhEh 


o  -    o 

££  £ 

flV  d 
d  d    d 

OOO 

OO   O 


0  o 

d~  d" 

1  1 
O  O 


ooo      22222 

S3  3    2  3  3  3  3 

OO   O     O   O   O   O   O   OOO   o 


OOO 

3  3  3 


OOO 

33  3 

oo  o 


io  co    t~      oo    oi    h    m    n 


o    . 
02 


k   * 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


345 


O  05  05  -p  05 
«2  <S>2  an  *>  <2 
O  00  co  =g  9  tH 

lo  m  <o  ^O  >o 

of  c/T  aT  »Tj2  tn 
03  C3  C3  C3  c3  c3 

OOOO     o 


x  CO 
lO  lO 


c3  53 


S-,    O 


<S  M  C3 
O       M3 


05  d 

ea  s 


^  05  05  05 
"3  03  03  C3 
££££ 


«i"d 

03 


o  o  = 

O  CO  lO 


5g 


LO  lO  LO  lo 


i-  lo  i- 


-h^h      -<M 


o  to 


O00C3N        f-tDfJNNCXSZ 


hMNM 


t^LO  CN  Oi 
OhM--        lo  CO  iN  X 
05  lO  CO  CO  04  CO 


I-  CO  A  —  -r  I~  t~  t-  -r  C".  —  — 
CC  t~  t~  —  t~  ~  —  —  X  CO  —  lo 

C-~CO   —   -rTH^OLl^H 


^t<  0}r-  CO 

§sss 


i'  x  =  o  £n  d  c;  f-  o 


is  io  ir.  S  co  oc  ■* 


o  i-  x  x  o 

(NINCOiNN 


O  X  CO  OC 
CS)  CO  LO  CD 
lO  lo  lO  lO 


■  h  lo  co  -r  co 

INLO 


lo  co  L-o  to  r—  lo  lo  i 


—  ;  . :  io  lo  o  n  m  lo  c  lo  lo 
X  O  ~-  X  —  x  —  X  01  —  — .  lO 

lo  ci  lo  r;  co  lo  x  to  j  ^  lo  « 


fl  o  o 


0 

-I 


1§ 

o  a 


'log? 


*  5    •  o  ft  *  5 

3 ^ §£25£ c 


^  c  o 


5g5   s5£S 


T3  "5  T3  "5  S^  si  d  fe 
-  co  ^  o  o3  C  .  .  •  C  c 


S&p  ftp  Sool  o  & 


5  fto  ftp  Co?  5  ft   ■  o# 


i  t--  X  O  t--      CO 


t-  CO  (M  LO 

6  6  6  6 


p  a  s  = 
c  c  o  o 

OOCO 


6  6 

2  2 

o  o 

a  o 


£    "7  °     ° 


'^-    V.    c. 

§9*5 


iffiJ 


o    o 


£    3; 

05      05 


©      C      o  C  O  OJ7     2 


05      05 


£  &  is*.0.  .2 


.2 .2 .2 .° 
2  22  2 

OOOO 


o    c 

3  2 

o  o 


.    oo    . 

2  22  2 

o  oo  o 


si 

«5  05 
># 

PQOO 


o  o 


■  0C  CTS        O     -h        CM     CO 


.2  .2  £MB£s 
o  o  assac 

■^  lo  CO  t-  X 


CM      CO 


S5     5zi 


346 


OIL  FIELDS  OF  CRAWFORD  AXD  LAWREXCE  COUNTIES,    [bull.  no.  22 


•sjajjEq— pnpoad  i^rai 


"cits 


b* 

02 


•;88j— mdapp^oj, 


•;aoj— x^dopno 


ran^p  aAoqe  apnrji^v 


iooo  oo  or:  co  cm 

>  00  CO  -"  CN  I  -  CO  O 

NP3MWOS<OMT|i«HO!fflMOOeO 


•Or-ltOrtMWOOCONNlC 
O)lOO>T)<tcOlOffl<DlO0Cj 
OOWMOOt 


KOCOOfflCO 


B8S   Avopq   8pn;i;iv 


liHOOOrHOJIMCOlOOfj'H^roiH  IfJ  00  H  H  •«"*  CC  rt 


paiBJ^ued  ssatuioiqj, 


•^98j— doq.  0}  mdaa 


U5O00C'-:  ~   y  —  —  -p  i-  o  t-  >-■  C  i 


O5(roiotooi03cotr>05co' 


ftftS 

o>  as  & 

■OT)  3 

WW 


S'-d 


as  o 


>•-  O  c3  O  O 
-^  ft  S3   O  ft 

So 


rH<N 

s.-ci-d" 


osoooocaooso 

<"").  rH    /-s    /-»    <*"Y  f*>.  i—l    /-s    <*V  (— 1    /^ 


8  5 

££  . 

MM   '.cQQQi^   iHSmmi^cQoci^    mpafc4^www^wwM 


O        Uffl00uo»0O«!0 

o      ftaooftftfloftflo 


"C  =s  rt  "S  £  m    'C  ps  rt  rt  •£  T3  s  n  'c  s ; 


cc  «S  ©  ^  2 .2 


COP» 

d  6 


o  o 

aw 


►; 

• 

a 

w 

C3 

& 

o 

o  o 

o 

[H 

& 

oo 

bo  w> 

fi  Pi 

o 

tJO 

C 

T3 

O 

o 

'o 

fl  Pi 

a 

a 

Ph 

W 

Ph 

©  <D 

o 

T3 

TJ 

TJ 

o 

c 

£W 

P 

f=- 

© 

© 

£ 

2 

ce 

S 

c 

c3  c3 

P 

2 

^ 

i 

e 

o 

£ 

e! 

rC 
'X. 

PI  Pi 

03    02 
OO 

| 

EC 

< 

C/3 

1/1 

< 

< 

i^ 

<N 

e<5 

&• 

ee  o 

SZ 

fl 

o    . 
3  o 

w 

H 

g£ 

1        DQ 

1      J? 

00 

s 

BLATCHLET] 


TABLES    OF    WELL    DATA. 


347 


K 

Poo 


£o 


O  <N  I 

_  ~   : 


TT   O 

S-   CC 


OO 


88 


~-£,hW£ 


©  «0 
"S3 


3 


8?, 


O^  KNN 


©  t  ■*  N  N  O)  K  K  L-  X  N  iH  CO  C 

ncocch  c/:  -^  i~    - 
cckcc^cc^cococoi 


OC'  t~-  00  oc  oc 


iONMNTHCJr-i«CC(NO:CMlNi-(MCO( 


ffiCONHMI 


ICD«OCQCQ00C4C*iOC400O>t^- 


ccococoe^oc'rrj-' 


■QMffiM 


00-HT)i0OrlrJi0Or-IHr-lrtrtrHr 


(MHiHrHOrCr-KTNrHNCC^KHl-lML'SOC 


iNCCrHHIOXl-IINnHNi 


—I      'OO 


©•fl-MCOr^CSNNHr-KNNW 


(NOCWi 


c  i:  c  l-:  i-  /  -  /  r:  ;  /  —  —  t~  c  — i  <m  ~h  i 


OCfOlOXrOlOOCCOiO' 


■  lO»OtOr~00»Ot»a>«>«Ot--a0< 


_    >OC«NTNNiffO 

■<CtCaWL-NXL-CCMeCK(Ot«(0®N 


^WMFh 


•^  <M 


-H  O 


o       oooooo         o 


c  o 


B     CS 

rf 

c- 

P- 

« 

ir 

o 

z  z 


c  o 


©   ©    ©    03       ©       © 

>,L.     U     h  S-.  t-< 

r*    C    O    O       O       O 

5m ww  w  32 


©  © 


•rt    -3    ^ 


©  ©  ©  © 

T31  T3  T3  "C 

>>  >-.  >>  >> 

b  s  a  c 

02  O2C0  02 


"e3  "e3 


p  c  o  o    o    o         o 

Sid 3 3  3  2      2 

<:ooc  o  o c_ 


OC 


.C         © 


348 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•s^jj'Bq— jonpoad  retirai 


C3  c3=Ot^ 


-  22?3 


>£, 


m  w  O  C  O  co  cc  O 


^22 


•^88j— t^dap  \*\o  j, 


•;89j— ttfdep  no 


tcm^p  aAoqs  apniijjv 


$  ifl  h.  !D  n  S  T  C  i-  O  M  M  N  N  C  lO  IO  M  N  H  ir5  io  Q  o  Ol  t»  t^  a  N  « 

anotonoir  i  — r  ic  — ■  r.  a>  ce  c — PSN«ocr.-iNxcu:x(rjOiN 


•}99J— J8A81 

cos   Avojgq   apn^piv 


OO»M00OHNL';i'OrtSHni!:OflrtMC««NM1'HHO( 


HHW^OOHNMLOQCrtNcOiOl 


•}99J— 

paiejiouad  ssgiupnix 


liONlON 


fOMf  ^ 


-r  >o  >-  C  —  — 


*199j— doj  o;  qidaa; 


O  CM  O  < 
O  CM  O  CM  CO  irf  c 


g  o  cd  c3  G"£ 
co<2  «  ^.2.2 


03  O 
2* 


A 

9 

A 

A 

J 

J 

J 

O 

o 

O 

o 

_ 

<N 

CO 

T 

•o 

iH 

cm 

I     £ 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


349 


55 


JS   £  -  m  , 


i-  co 


co  O 

o  c 
°°8 


CO! 


re  I- 

CO  n 


3± 


83   O 


5"  WS 

tea 

OoqH 


s   § 


oo  to 


iO  CO  ^f 
C5  —  CM 

»  i-  bo 


2gg    2 

O<CO0        CO 


—  I-  CO 
t^  o  co 


safCCCXTi-N-'  N  -r  O  1^  'T  M  O  O  O  li  ■>i"<r  «  h  'OCXCO  —  CO  M  lO  o  a  ^  N 
PPIOXNCSCr.N  I-  O  '/.'  C  M^  a  C  '1  l>  r.  N  N  N  T  Li  O  S  N  00-*-  00  l-  OS  OC  CM  X 
3t>.T)<NiH05!C'')iCSiH        M«NOMMNO©MNrHt1C>        CO  CO  CO  CM  1-1        PS  ^H        CO  i-i  Ci  CO  CO  CM 


i-l  C  3s.  "H  N  !C  IO  U5  ul  C  N  X 


iijiffliot^McDLlXta        30  CO  O  CI  CO  t-  CO  i-1  il  i-1  —  —  C  C. 
I  CO  0  —  CM  O  ©  OJ  O  CM         CNCCNS  cNM-iJ:  TCNCN^IN 

t^  O  M   CI  Li  /.    C   H  CO  HHNf  HHPt^XHN«HLl 


LI  V  Ol  M  1^ 
0C-H  —l  CM  CO 


IC1Lli-lr-IC>TCO-tf'00T-(CMCO< 


Li  ■* 


O  O  *f  li  35  Q  co  <N  co 


Nt^tOHH, 


lIO        O  CM        .-I 


iOCCOJ^NI 
O  CN  iO  N  X  ( 


C1CNCNM«rtrt 


CO  CO  t~  O  < 


O  CO  CO  r~  00  CO  i 


LlOOCiUCOCOGOOCOCOO-OOCO 


g*    §£&§  :  ^ao8 


>»*s 


t>»g 


>*    n    n  n 


r?         "^ 


CO     "f     CM  t~-     CO 

6    6    6  6    6 


HEEEE 


CD 

T3 

T3 

ffl      CD      CO   CD 

i 

c 

c3     ccj     c3  c3 

fl 

c3 

C3 

OH 

> 

> 

>    >    >> 

> 

o    o    o  o    o 

O   O   CO   o 

li     CO     r-  X     CO 


350 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.       [bull.  no.  22 


■siaxreq— ^onpojd  i^iui 


•^88j— tftdapi^oi, 


•loaj— mdop  no 


O 

0 
+j 

0 
o 
O 
I 

.9- 

CO 

8 

© 

o 

eg 

t 

$ 

o 

<D 
o 
8 


■^99} — anejd 
mrvvepaAoqB  gptv^jy 


■B9S   Mopq   epnmjv 


•qa&j— 
pQ^j^ned  ssaa^oiqj, 


•?88j— do?  o%  w&da 


g  ©  ©  cs  g-£ 


DQ 


a>  © 


"c3~c3~ 


I  r-Trn"  ©   ©    © 
'      ~     -  .2«2<2 

!  a;  S  cc  o5  o 


>^^r 


<N  -r  <M 

CO  00  CO 


c3  fl 

1*8 


.JHMOC'NOnONNHHTTINIl^Hif 

^c^i^cNcoc^Tiico^c^co^coTric»^cO'^^ooi-iCNcoicoOi-iC<ieo 


OiOOONt^OOMOO)] 
nOCOHH         OJOCOH         i 


•OOiOOtOO! 
I  i-4  C5  CO  <M 


OOOi 

HOtO! 


OifliOOMOOOOINiONI-nO'ONfflOOOOOONOi:   Iff   ■-. 
-     -iOHO«CNO00HN-HNNHH<i<ONf-  ~ 
•  00  CO  60  05  CO  CO  00  CO  05  CO  CO  " 


i  CO  CD  CO  00 


a 

Is 


blatchley] 


TABLES    OF    WELL  .DATA. 


351 


c3      ^ 


^  c  o      1= 

OdT3         © 

z  :  :    ^ 


o    •«     © 


2-ldS 
4- 9-s  •&« 


to 

3 


Ss 


OCX'VOXNMNNC-/    X)  ■ 


CO  CO  CO  i-l  ' 


OtO'J'CONfMMi 


l<N  COlOOO' 


I  CN  TP  00  i-H  CO  ■*>  00 


HHHCCO' 


x~x— c:cr.  cnojco 


18^2 


NMf       •-*< 


OHOOOMOOOOi 
O  t>-  GO  OJ  CO  lO  CD  C 


c-i  o  o  x  ~j  x  —  =  t- 


lOOCOOi 


s-d 


5!   ^d    si  "5   S 

°  <s  o  r?  °  <s 

ftfi  O^  P<C 


^  ©  °  So  2  P  ©  °  So  2  ^  ©So  2  >  °  So  2 

■-  2  °  C  3-h  2  o  c  s«  g  s  s«  o  G  s 


o 


o  o    -^  c  ft 


p.qii  .'11  -:£ 


N 


CC  X  o 


o  o  o 


(O  <D   © 

d  'd  d      _r 


fc     £     £     £       £ 


o  o  o 


3  o 

■SO 


53« 

CJ  o  o 

3  3  2 

o  o  p 

£££' 


o  |o 

"c3    '"c3 


•  O  G3  o  c;  o 


►3      ^      £      J  J 


T      OfflNCC         03         O 


Ifc 


352 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spjjeq— jonpojd  xexwi 


•^88j— mdep  ibioj, 


•^9j— i^dep  no 


>o  >o  <n  ^3 
c3  c3  c3^ 


©~T 
IO  CD 

i.O© 


ON  CT> 

CO  05 


•r  cc 


5  ©°° 
rt  o3^ 


©'d 

"c3  O 


££ 


OMtOO 

IO  i— I    t  i-H  i-C 


CO  "O  iC  "O  s.  -c 

O  M  h  O  f  IO  I 
IO  1C  O)  CO  O  (O  l 


•}88j— airejd 
ranjBp  8AoqB  apnmiv 


CO  >0  'O  I-  T  -r  W  <N  N  00         CN-<fCO-^-H"<r^t^cOcO^H 


OOOOHNNCOWNNrtO) 


O  rr  CO  ■«*<  ■ 


589J— ]8A9] 

bos    Atojaq   apnimv 


iOt^OOO^t^O-»j(        tp  i 


■  ooiowo^ifj 


-J98J— 

pa^j^auad  ssaujpiqj, 


i  Ol  00  00  CM  05  CO  CO 


•^88j— do^  o;  mdaci 


«o  CO  t>  IO  00  CO  iO  ©  kfi 

HiOO«0>NiO*1"-w        w.  -~  -»  -»  -»  -  -.  iv-  w  »•«  -*•  -^ 

ffliONU5»riOaCNiOO)        X  iO  Ol  N  'O  IO  a  M  O  (O  O) 


i*005  0JHCON»X« 


'  >0©C© 
>  1<  >ri  O  ■— i 
i  iC  CO  iri  >o 


5^ 

c3  o 

fl  o 


O  c3  o  O 

—  c  o  ft 

&  *  £  ~ 


oOoJoo'oio 
o  ftrt  o  o  ftd  o 

.  *  §>  2  *  *  a|  ► 


fto 

55 


0000     N     NN        CM        CM 
00  r-     t^    CO  -"J"       CO       CO 


CN      CO      © 


7* 

©CO     f     NH 

'3, 6   6   6  6 


lO     00 


•  -  >>  >>  >>  >> 

O  c3      C3     C3  03 

mO  O   OO     ( 


o 

©    ©    6    -- 
>^  :*;  £  ££ 

(S      IS      S     " 


so      c  c  o  w 


o  o 


KW 


o  o 
££ 

C3  eJ 

tftf 

WW 


03  O 


33  © 


I-     ', 

3    . 

c  c 

d 

03  03 

a 

fc  6 

o  o 

o 

o 

o 

o 

o 

o 

S-i    t-, 

u 

o  o 

*P2 

d 

,cc 

J= 

.d 

,fl 

A 

A 

A 

B. 

j=l^ 

CQO 

0 

OO 

o 

O 

o 

o 

O 

O 

o 

mm 

tB 

OO 

©© 

tNCO 

CO 

t— 

OC 

(N 

CO"t< 

ir. 

CC  t- 

BLATCHLEY] 


TABLES    OF    WELL   DATA. 


353 


mo 


>©  ^< 


IliS- 


CO    CO    CO    CO  - 


,  OT  >-■  o  o  wTc^wco 

j  cJ  CCO  ci  o3  oj  o3 

>o£  :  :oooo 


S:3 


03  c3©© 


O  ©  co      .OO 


88 

coco 


OH5       '00 
t-©        •© 

iO  CI      '  OS 


©  ©  ©  lO 


s_  -a.  y.  seoosxHrt. 

(O  H  to  ij(  01  iO  ?5  O  f  f ' 
dOtOVMON'fON- 


O        OOCOOM 
CO        WNHOO 


LO  I O  BO  DC  GC  0^  CO  00  00  CO 


NIMNNHO^NOlCSOONCONiO 

MOOMlOOOtOCOLOOiOiOTfifflON 

cN'<*<ooo^H-«<t^O'9,r^o^TtiTtiioTj( 


O-HiHCOCM 


CO  CO  1-H  lO 

00  CO  CO  r— 


O         ©<M  f  OGC 

r-      10N0000 

"Ctf        NOONC3 


to-^TtftNcMCMcMCMtNTti 

OOOOlOOONHMt- 
■*  •*  N  O  O  1"  ^  "3  N  O 


:88S838i 


COOOOiOCSt^OOOONNHN 

ooo«-  '  -  ■-  ::  to  ■_:  to  '/  n  73  r:  -i> 
t^©COtOtO©cNtO©cMtO©©©©© 


*  N  (N  tO  M  ^ 
to  1  -  r -  1-  to  :o 

O00»0t0  0) 


1;  a- 

O  e3 


1 173   s_   S3 
,  o  O  C3 

)  o  ftrt 

IMmm 


O  °  03 

O  &a 


o  P< 

.g-d  O 
•-'CO 

^cq  : 


73  o 

cq  : 


:^e?cq 


c 
o  o  o^ 

:  :  :w 


fl  o 

r-i  <*     ■  CP  y 

S.fcJ-d  £0 


■CO 

cq  : 


mM 


o-d  o 

•d'E-d 
'.CQ 


a  o 


3        3 


>©     -T     CM©  O©00< 

1  co    cm    r^  t^  t^  t^  to  ( 

1  tO     to     •*»•  ■*  T  ^1  tji  • 


Tf  "CflO 


ICO    N    t 
OOO      O66666O 


OOOOO 


££  £  KKKtttt  £  ******* 


'  O    O  +i".+3"+3"+3  +»'  Oj^GlCU&l&lO* 

,d,d    .E)    .3  J  J  Si  X3  3  3  3  co  m  to  Eo  to  to  57 

tJobi   w>  wi^ "  fcio tiblo m  m  ,2.2,2,2,2,2,2 

*CD '©    *S      ©  O  O'J'J'S'S  "3  773  7— 773  73  77h  7— 7774 

jj  _5  ^ j^h^i-}  ,-)  OOOOOOO 


*d 

.22 

S3 

773   >> 

Otf 

►4o 


.Q.O. 

C3& 
SS 

00'    o    or^dooo  d   Ph^P^P^^^^ 

32  2  3  .  .2222  2  .y.£f.£c.£P.£f.Sf.£f 

OO    O    O^^OOOO  O    CQ  CQ  CQ  CQ  CQ  CQ  CQ 

CO-fl1    to    to  h  y.  o  o  —  CM  CO    •— l  CN  CO  t  c  to  f- 


S       d 
o       o 

ho       bXi 


o      o 

.3    2    3 

cqo    o    o 


©  i-t         CM         CO  Tf 


23  G 


354 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siajj-Bq— ^onpojd  \v\iui 


S  c3  03 


CO<M 
■Oi© 

IOOO 


© 

© 

'is 
Q 

i 

o 
to 


•}99j— mdap  i^iojj 


oi  o  o  i.i  o  o 

~r  *f  -r  I  -  r-  o 


•:j99j— q^dgp  HO 


fOOMI 


•^99  j — gtreid 
uirrvep  gAoqe  9pn;piy 


2<  O  CO  <N  re  co  ■>*<  ( 

OO00r-IH®N^ 


tDNt^<Nffl®N05MaO®        I  ~  CO 

lO^m-t-iMO-t'j'fflcooo      -ho 


*^99J — J9A91 

■B9S   Au^gq   gpmi^^v 


OHCOOHMiOL^OlNn^KOHM       0"^l^O-^< 


t00M00f-1<0C«NiHO*         CO  00 

•^t^pioooco-tf'iiiocorf'^      ooa> 


•}99J— 

p9^j^9U9d  ssgujpmj, 


i^NOMH 


hOWO«i 


•J99J— do;  o}  q;d9(i 


iOfflOOiO(OoeONiOM»05MiO!000        -*05(Ni0  01INiCi0i0NN50 


.70^0 


■B  9«  G  P 


"■sg  ssf-s*  s 


p.  fl  =1 


8>2t*§?8 
3;~  2fi 


oOcJoOSo 

O  ftfl  o  ft  «  o 

2  co  ca  2  co  pq  2 


:co   :W 


d  : 

111 
111 

co    W 


i0)    i     .     LlJ 
«2«2  *>  ^.2.2 


!M  1.1  OC 

!  3  3  S 


CI  CO  -H  1-H  <N 

d  d  6  6  6 
£££££ 

0}  G}  C?  0^  c? 


ooooo 

J  J  J  w  H 


££ 


o  o      o 

3         2    2 
o         o    o 


2  2.22.2.2  .2 

2  22252  2 

o  ooooo  o 

w  ■* «« «o  i-l  c<  n 


BLATCHLEY] 


TABLES    OF   WELL   DATA. 


355 


1-1  w  d  m 
O  03  O  o3 
55D       O 


C 


O     £ 


35  gd 
Ilg 

!>  03  © 

w    55  . 


Z* 


<     d 

:Sg 

^•d 

r    a 

.-C3 


fio 


Aft 


ft 


tH  lO  ■*  lO  00  CO  M  ffl  -hNM 
U5  t  C  O  N  iO  O  M  CO  Tji  lO 
C  O  O  O  O  O  t~  •V        O  t^  •* 


—  i-  z  t  c  r.  f  «  1 1 
c0wcoco-.£cococoeo< 


c  -crc  >~  l~  u-  m  oa 
iocoocococoocdp: 


oCNTfL'; 

O  l-O  CO  CO 


O  ifl  to  ifl  N  N  l^  f        05  00  CM 
■q<iOCO-*,I^-^l-^10         O  lO  f 


X  to  CO  35  — '  to  -—  >~  ~  CO  ro  :c  X  O  CM  -r  to  ~  C5 
O'Hi-lL-tOiO'HiOMClfCiC-l'n'Viffl'O 
HO0HrtMrttHHH(NTI>0O'9'H00H^XH 


— ■       '^O 


t^OOiOCMOOr^ 

NtONOO-HffltO^ 

C5  ci  a>  oi  o  o>  cm  io 


06  co  eo  < 


d  o 


Sg'g 

ftd  O 
d£.* 


O  O  O  O  O  O'0. 

'd  d  d  d  d  d  3 .. . 

:'::::  :cqW    caecbd 


C-dd 

C300 
COO 

if** 


d-d  ^jd-d 

03  o  O  O  o 

d  o  o  o  o 

£3255  ~ 


ogS'g 
ftp  fto 

-■is* 


WWWM 


gd^  g-d 

on  °  «  o 
C  o  ftd  o 

:*£&;*£ 

;  d-S'C  d-- 


o    ^ 

ft 

•Oo?£  o 

"E  >-.d,d 
ftcefc4    I 


U0  iO  iO     lO 


_  o 

Is 


d  o  6    c 


ftftft      ft 


o    5 

£  fc 


o  o 

55  55 


C/5    CC 


^Fh 


O        O 

55     £ 


6       55 
55      -e 


CO         T-H        CM        CO 

c      6    6    6    6 
55     55  55  55  55 


03     03     03 

-a   a   a 
d    fl    d 


.d.2 
.53  .d 
ftO 


.222°  ° 
223  3  2 
ooo  o     c 


t>  o 


gg 


t/5  </3  C/5 

i  ©  ©  ©  © 

©  O  ©  O  O 

d  d  d  q  d 

*d  'd  d  d  *d 

c  o  o  o  o 

_  _  -  - 

ft  ft  ft  ft  ft 


<H  <;  <j   <j 


i-l  CM  CO      th 


CN  i-lCI 


C-     i-l     CN     CO 


CO       03 


6= 
1* 


356 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


<p 

rt 
"•£ 

rt 
o 
O 

I 

5- 

.8 
CO 

8 

O 

8 
o 
.Co 
8 
8 

Q 


•spxreq— ^onpoad  repini 


188j— mdep  ib^oj, 


'?93j— mdep  no 


•^89|— ou^id 
ran:rep  8AoqB  epn^i^v 


•}89J— I9A9] 

■B9S    Avoj9q    gpn^iv 


•189;— 
p81Bj^9U9d  ssgujprqj, 


•?98j— do;  o;  q;d8(i 


!      a 

-t-s-u 

•■^TJ 

-L-)  -+J 

•  -^> 

®  s 

".©  s 

•  <M     OJ 

©  (I) 

'  © 

oo 

,'OClo 

•  "£°< 

,00  05 

:a3« 

.  .©  -"-'  s- 

o 

a?  ^~_J~ ©    ■  _T  © 

+J  4J  .(J +J  .|J +J 

1, 565  f 

water, 
water, 
1,560  f 

water, 
water, 
t 

1,575  f 
water . 
1,575  f 

water, 
1,572  f 

water, 
1,610  f 

:    £* 

986  fee 
954  fee 
978  fee 
999  fee 
977  fee 

987  fee 

••   # 

c3  03  o3  o3  c3  c3 

•  OcqcqO    -mm 

OgqOcgcoO    .coO 

•       GQ 

oooooo 

•  m 

o    • 

t? 

CD 
CO 

"3  :  >» 

fr  :   8 

iO  coifl'O  co  en 

ci  eSCNtN  es  c5 

a 

;fl 

p  • 

O          OO 

o 

£R 

r-  io  O  O  t—  O 

<N  co  <N  cooo  o 

a 

•       O 

o 

CD      •  O)  Is-  Is-      •        CD 

00)00010) 

I*"1 

"~,,H 

■1      .  1-4  1-1 1- 

:    'H 

1-1       r~"~' 

CN      • 

,_i 

8 

.lO 

LO      • 

lO      'LO 

LO      . 

>o 

•lO 

OO 

rt 

.rt 

t>-  co  o  co  t  co  i 


J  CO  >Q  CO  00  <M 

a>>ococooooooo65c^oot~- 

CO  CO  CO  O  CO  CO  CO         CO  O)  CO 


NrHlOOOlHr-ICO- 


lOOMHHt^ViONWOC 
OiOHC5hht)iNNhN 
HHHlCOOHHlOHKJl-l 


oeooHowo      ioco    'iO'Onocoh    •  o      co 

C)  f-i  00  00  CM  CN  Tf  lO       CM  •  O)  <M  CO  CO  »-l  O      •  .-I 


oioootoMoo      io  o  o  < 


LO         OCOOOCT)lOCOCOl 
O)        N"OO5CNiOU5N00 


i  lO  LO  rt<  O 


l  CD  lO  O)  CM  lO  LO  O)  lO  0)  LO        LO 


3  o  ©  c3  fl 

gq-2  ©  >.2, 


o  o 

ft  ft_3 
©  ©71 

cam 


'o  O  03  o 
O  ft  fl,  O     •  .  •  77, 
fe  ©  03  fer      •  **>o 

^'d'S^  O  ©o 

4»-c  a  h'O  2© 


O  O  O  ftd  o 


o  2  o 

o  ft  o 

* "' 


£  3  .fcj  i3  £  .Jh  •; 


'^^44 


'^mraM  :£;g    'm'm'MoqwS  :S'^wM    M 


lOOOcOiO 


CDCO<M  00  t~-  LO 
l-iOI>05LOOO 

0)0)000)0) 


-O  o  o  o  o  o 
*r^  rx3  'C  i3  'd  *d 

co  :  :  •:  :  : 


CO  t^  OOO  COO 

LO  LO  LO  LO  LO  LO 


£  55 

I  © 

>  m 


o 

•^  s  ©  ^ 

©     o3     S  _-. 

J    fl    -£  -d 

•     ef ■    ^  © 


o  o 

o        o 


2  § 

O   Q 


9    I 


OOP 


ft  • 

03  O 


©z 
©^ 


I     5 


rt<  ^(LOCOtN 

6  6  6  6  6 
^^^^^ 

^    u    t.    ^    tH    O 


tS  hi  J  |j  (-2  CQ 


o  o  o  o  o  © 

222222 
oooooo 


J,«    J.525 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


357 


co  co 
03  03 


'^_-0>Oi03 


03    |$l 


7*o3coo3o3o3o3o3o3o3 

bO    ooooooo 


rr-J    CD    CD 

.cd^c^S 

!£§»§§ 
L°i  -/2^ 

■  co  co  ►> 
03  C3  t> 
OO       OO 


co  co 


co  o3  co  co 
03  co  c3  03 


^    CO    CO 

O  03  03 

ZOO 


NlfliC 
l_-  GO   C 


CM  iO  i 

CO  t» 

©5  Oil 


CO    CO    CO 

OCOt 


si 

03^ 
CO 


CO    CO    CO 

ooo 


WOMCOO 


o  o  o  to  o  o  >  o  io 

o  «o  i-4 1-  l~  ta  EL  <o  i— i 


OOOO        OO 


IO  O  O  O  CO        <M  i-H  LO  ■ 


fiOHiOOi 


COCN  iO 

r-oo 


o  o  O  OO  t~  rp 


Nij'OfMnHcuo 
o  co  io  co  r~  t~  00  r-  ~r 

OOOOOOOOO 


UNMOOR 


-r  O  GO  O'/CI-Ml-C  iO  WOH 
I1  H  N  l/J  K  u-  ■;  -r  C  C  M  M  «  f 

oooooooooooooo 


rf  ■*  t-  OJ  •f  t—  t— 

-HOOHOOOTfN 
OtDVWHOO 


TP  itf*  -*f  Tjl  -^1  £>•  O  "^ 


"   iO  M  (M  (N  w  N  O 


Oi-iCC*' 


SSSS^SJ 


OOHWOOO 
CO  O  iO  OS  GO  O  o 
C-.3KS010WO 


N00O)iOiOO>CO00H 

os  oi  oo  r—  co  io  uo  -f  go 

O  O  O  O  O  O  O  C7^  ~- 


OlOHiOO^NNiSOi 


OOOOOOOOOOOOOO 

m  ::::::::::  : 


OiflUJiO 


lOiOiC»OOlC»OiO»-0 


<Mi-l< 

CO  CO  < 
iO  iO  ' 


)  r-l  CN  CO  IO  lOMCDOiWOOOSOS^NcOMN: 
I  CN  i-i  O  C>  OOOOihhhhhNNNIN 
)  IO        >OlO        •*!        TfiOL-JtiOiOOlOiOiOiOlOiO 


HlOSlH  l-H 


Jod 


OOOO 


<s  co  <s  cp 

OOOO 


OOOOO     .,    .,0  fc* 

o  o  2 


O     .  o  o 

tf  i-tftf 

gco  §g 

« « a  s 

«-.  o  r  u 

'd'^-S'O- 

1=1  -?  d  1=1 


©eoes<»cpoo®y      S  ©  w  s 

ooooo°°o>    >o>> 

CO*  02  CO*  CO  CO*  K  H  CO*  )-3       i-3  CO  03*  1-3 


o  o 

££ 

03  03 
SS 

<0  CD 

03  03 


•      •      •  CO  •f  <M       ' 

oo  to  co  i-i  i-h  i-i  -w 
_co     "ododdodddddodd 

Q      •"■ ,o3o3o3o3o3o3o3o3o3o3o3o3o3e3 

h>*  >'  oooooooooooooo 


oc  CO 

6  6 

Z2 
a  a 


OOOO 

2323 

OOOO 


oood 

3322 


.*  .2 .2 .2 .2 .2 .2 .2 .2 

J3  A  r^  £X  ~  A  -=  —  A  r 

ooooooooo  oooo    oo 

t-  00  a>  O        ^             NMifinONXOiH  CNcO-^uo        CD  !>• 


o  o 

22 


°  ®222c'222,222 

2  £22222222222222 

o    ^oooooooooooooo 


lC^^cO'^,'Ocot^ooo50>-lCNco•<», 


i-i      CNCO 


358 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spjJBq— jonpojd  I'eiirai 


•%QQ}— mdep  p^oj, 


CI 


03O  c3' 
O      C5 


o  E 


c3  O 


<2«2  <S<£  <2<S 

N  K>  O)  10  00  O 


c3  c3  c3  c3  c§  03 

OOOOOO 


'WOViO 


09 


:  - 
•  <y 


o 


«2«2«2«2  »  ^«2 


-!^  £  ^  ^  <°  <°  "^  co  «5ooffl^ 

-i©  g  O  03  0>  Ol  CT>  Oi  ]£Ci  "g 
ww  *"'  co  en"  t/T  </T  »T  wT+f  wT  c/T  cS 
C3c30dc8rte3c3  £37*  S  d  k 

OOZOO  O  O  O  O  02  O  O 


COflH 


-r  -  ri  r-  it  —  >T  o  c 

»oooa»ooc 


•^aaj— qjdep  no 


•laaj— 9UBid 
umyep  3Aoqi3  apn^i^v 


•eas   Avopq   ©pr^i^y 


•aaaj— 


•}8aj— do?  0}  qidaa 


a  o  o  cs  e3 
02,2  ©  >.2£ 


SZ 


53  o 

I" 


LT>        CX 


-"  'T  CO  ~   —  O  '-T  i.O 


O       OO 


r-i  -p  x 

•-    ".O   CT 

oo  o 


[^  N  1^  rf  -r  a  w  co  oi  N  lo 


0  00<*lO«!CLOCIN 


LO  IN  O  lO  •*  ■*  l 
t~  GO  <N  CO  <M  i-l  i. 


iMOi^O' 


MNt^Mi 


!8S 


•1-NOOrtiCcoiON-H 

"ti-owo»a)Mio*H 

'05CTiOCi0000003iOCT> 


Oi  Oi  O  O  O^  OS  O^  OS  c^ 


T3  O  O 

ca  :  : 


■gs 

P  to 

TJOOOOOOO  O^t) 

■g  t3  t3  TJ  t3  -d  *d  *C  -O  .fa  •£ 

pq  ::;::::  :Mpq 


tJoooooooo 

pq  :::::::  : 


S8 


00  GO  l~  CO  t^  1^  I 


■  00  t-  tc  to  tc 


'  tP  lO  iC  U5  lO  >0  iC  ' 


Nrtcc.««rtrtr-i    ;    ;    ;    -c^co  ©    —  ©  £  °c  ^ 

ii^S°m^.'^^-6  6  6  6    6666666***°°.' 

2~2~.2~.2  2~.2.2~.2       -     t^t^  t^  tZ.£££tZ£±r'r^     ^ 

g  gS33«S3ssr.  krb  J  S  S  3  '5  '5  3  '8  "8  '3  '3  9  ?  r*  ? 


ooooocoo 
,      £  ^fnfufufupufufafu  £  £  £  ^  £  £    ^    ddddddddddd 

3    32.SP.Sf.Sf.SP.£f.Sf.SP.£f322S2S  3  23323333333 

o    oomcameocQcapQcQCOoooo  o  ooooooooooo 


iOSMXiCOhNM' 


>.T  5C 


X 


3 


BLATCHLEY] 


TABLES    OF   WELL.  DATA. 


359 


"So 


©  ^ 


7i  09 


c3  w 
O 


©So 


©  ©  .-,-©< 


c3"-0 


iMO 


»V1    I" >*" 


-3J5- 

■  C3  c^ 
!  co  c3 
i      OC 


o  :o? 


i-h  o  3  cm 


w  o  o 


x  x 

?:5 


§2 

O  EC 


r.  ~  — 

©  *0  © 


©  ©  ©  ©  © 


.  ©  ©    •  in  oo    •  cm  oo 

■Tt<CM      .  O'*      -or  co 

iffloi     •  ©  © 


r--  r—  co  cm  ^r 

ooooo 


o  ©  o  t-  ■ 


©©©^©©©•^©GOrf©©^©©^©-?-^!^ 


421 
429 
434 
472 
453 
456 
1, 068 

473 
461 
461 
786 
1,065 

CM  CO  —i  ©  ©  ©  CO  "X  -h  X    X   ©  Vj 

rr  i~  co  ©  >o  co  io  x  co  co  co  t^  to 

■<f-^Tf<t^©Ttl-^<TjiO-«<Tj<-<J<© 

^  © 

LO  00 

©  ©  ©  CO'  X  -r  -p  — i  -r  a  ©  CO  X  IO  -r  -r  co  ©  lo  CO  t~ 
MOioi-t^n'''  ©  CM  co  ©  -r  x  X  lo  -r  co  -r  ex  co 
■VTT^<©TriTj(0C©'^-^-V©-*i^Orf<'*l©^f©© 

cm  lo  i>  lo  — ■  ©  to 

00  LO  I-  CO  CO  O  CM 

-H  lO  IO  ©  © 

CO  CO  CN  CM  00 

CO  X  i-0  ©  T  ©  ©   —  ©  ©  ©  "5  © 
■^COCO^CNTfiLOCOCNTPCOCNCO 

t-~  i-O 

CO  © 

LO  t^  t~  ©  ©  ©  LO  CN  LO  O  0C  LO  LO  CM  ©  X  ©  ©  X  CO  1^- 
i-t  CO  CO  CN  IC  LO  CO  CO  a>  i-H  CO  -H"  CM  CN  CO  T  t~  "»>  t~  CN  CO, 

i-  ic  co  os  ©  'O  io 

—  _  ,-  -y   .-  t,  x 

©   ©   ©    ©    ©    ©    LO 

992 

975 

975 

1,300 

1,579 

IO  CO  i-O  ©  CN  O  ©  ©  CO  ©  iO  lO  -r 

io  co  co  ~  ©  co  i-  x  re  co  io  ©  tji 

©©©coio©©©Loo2©©>-o 

CN  LO 

•*r  oo 
©  lO 

'0  i-O  lO  — -  —  ©  ©  t^  CM  CO  ©  CO  L0  CM  —  LO  iO  —  ©  t^  ©- 
CM  .0  i-O  CO  CO  —  CO  I  -  ©  CM  CO  ©  CO  1-  t~  C-  CN  LO  OJ  ©  — < 

©  ©  ©  LO  Oi  ©  CO  LO  ©  ©  OS  IO  ©  ©  LO  ©  ©  "5  ©  LO  LOj 

I  o  c£ 

:  :  :W 


3-c 
73  o 
3  o 
2£ 


>a  c 

ffl  : 


■d  r 


•o  j- 

°  2 

o  & 

>    © 

!>  be 

-Wd   O 

^Icq  : 


- 

0  M 


-3  o 

PQ 


O.M 

"3.3 

bd 


S  o 


o  o 

O  ft 


9^  Jr 

do° 
3  O  ft 


t3  i-  .-a 
o  o  ,  o 
o  ft  •  o 


CO     t      •    »^    0O     •    (-•    ^*    bO     ■      •    *"    &/'•"" 

pq  :  :wcq  :pq^pQ  :  :W«  :w 


91    * 


jc~ 
c   C 

ft  o 

CD   i- 


©  ©  i-  ©  © 

t)<  LO  LO  lO      i-O 


—  — l         — i  -HO 

lO  LO         IO  LO  LO 


oo    o    ©    r^    r^  i 

©     O     O     OO     00  : 


OOOOO      C 


o  o 
ZZ 


rH  CM  w* 

6  6     6 


TJ«  -H       -H       CO 

6  6    6c 


ZZ     J?     ^^   53   S5 


55  53 


T3T3'0'0'0    -O         "OS 
3  3S3  3     3  33 

OOOOO      O  OO 


E^E-HEHft 


3  3 
o  o 

OO 


2  22  2  2 

3  33     3     3^ 
o      o  o    o    o,* 


o    o 


6    6    6    6    oododco' 
Z  53  53  53  ZZZZZZZ 


t^ft 


HEh   FH    ft3^ 


3     3 

c 

3  3  3  3  3  3  3- 

3     3 

fl 

3  3  3  3  3  3  3 

©     © 

© 

©  ©  ©  ©  ©  ©  © 

O  - 

O  O 

bo  bo 

3  3 

3  3 

cB  cB 

©  © 


o  o  o  o  oodoooo 

O  O  O  O  OOOOOOO 

bfi  bO  bO  bC  b0bCb0b0b,)bCbjC 

.S  .S  £  .S  .9.S.9.S-9.S  9 

'S  3  3  3  3  3  3  3  3  3  3 

CB  C3  cB  cB  cBcBcEc3cE©cB 

©  ©  ©  ©  ©©©©©©    o 

pj  «  «  tf  rttftftftftfsj 

c3  c3  c3  c3  c3c3o3c3c3c3c3j 


2  2  2  2  2    ° 
33233 3 

OOOOO  o 

tN  CO  -^  lO  ©    I- 


2.2 

33 

oc 


2.2 

oo 


o      o_o    o    o  o    o 

3    32 3  33 3 

o    oo  o  oo  o 


LO     ©     t^  00 


2      S      ^ 


33  3  B3S33S33333- 

©©  ©  q^c}©©©©©©©©  ®l- 

o  o  o  o  o  o  o  ooooooo- 

CNCO  -V  LO©I>-00O5©^CNCO-«,LO>. 


3G0 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spjiBq— jonpoad  veijiui 


"IW}— qjdap  ib  jo  j, 


•J88J— qjdap  po 


J89;— QWB\d 

ranjep  8AoqB  apnji^y 


•J88J — I8A-9J 

■bos   Avopq   apnjijjv 


•J88J— 

pajBJjauad  ssaujpiq,!, 


•J99J— do;  oj  qjdaci 


;  P 

:  a 

'.S 

•  +j 

•.t^ 

.+3 

© 

-w 

•  P 

:  p 

..J 

•  P 

09 

;o- 

:c 

09 

5 

io1 

oc 

o 
© 

■«2 

4J 

-t- 

+- 

!  a 

+- 

•  © 

;  © 

8 

co  *_ 

.'  © 

i 

is 

09 

Si 

!o 

©   09  ©  ©  <E 

ffl  o)  o  o  « 

:«2  <u  a 

■  w-s.2: 

:S 

!►« 

?S 

+-.«. 

,-j^ 
►  » 

-111 

O  CO  lO  00  OC 
lO>Hrt(NcC 

.    ico^f 

.  1-H  OS  O" 

ana., 
s,  917 
twat 
s,  1,55 

<?  942 

03 

iq^j 

■U    rs 

c/i~  c/T  c/T  c/T  c/T    .  wT  cT  ly 

""     •    CO 

•p| 

•  03  cr 

c3  c3  c3  03  02 

•  03  03  « 

•  03 

w  o37*  o3  o; 

■  03  cV 

c3  c3 

coC 

■  o 

ooooc 

:ooc 

•  o 

OoiOC 

:o 

O 

= 

"O 

ooo  oc 

•0«3«- 

R  : 

■  wt^ei" 

ura 

:8 

c 

■  t- 

lo  CO     •  (•-  O 

"-HCOTt 

•  t~-  00  t^ 

•  CM 

r--  CO       •  CO  CC 

Old      'OiC 

■  iO 

OS 

>~   CT 

'  o 

CO 

CO  O 

\  T~l 

I1-1 

;  rH 

1-1 

I"-1 

'-' 

rtrH 

~ 

•  t~- 

CNt  CO  lO  i-H  ■* 

•OO0C 

•CM 

CM  i- 

(^ 

■  lO  TP  TP 

>0  -r 

Os  0->  Oj  Oj  O 

•looo' 

OS 

io  — 

•  lO 

lO 

lO  OS 

I'-' 

'.  "^ 

'.  r~' 

1-1 

'.'-' 

1-1 

1-1 

10  rocs  ir 

OOttC 

CO  00 

co  i-H  os  r-  i^ 

00  <-l         00  CO  lO 
CO  CO         ONT 
Orp         OTTO 

COCO 

o  ■* 

O  tji 

OOOOOO-tfOC 

O  l>-  -*P  O  O  -f 

i-o-H        r- 

'~H 

Hrirtrt'" 

^H           1-H  i- 

1-1 

*■*        •"■* 

rt 

H              '-*'-• 

lOCDOlC 

C^tN 

NO)i-IMCON"0'<fNO'fl' 

TP  t--  CO  rr  CM  CO 

COt"iOOtOOCOiOiO'*CD 

■*«N>OCON 

T*^0<* 

*o       -VC^ 

-1 

^ 

-1 

rt 

^ 

-1       rt 

00r^^<N(N< 

OO        O  00  CO 
CN  CO        CO  <N  f 

COCN 

-*  lOiOCOCN 

CN  CO  »C  CO  CO  <M 

CDOJrHH 

CO  CO 

N  ifl  H  o  o  o 

l>C0"O'J0  00NO00t^ 

O  ">r 

CO  TH  OS  CN 

•f  CO 

O>0>05  0" 

OS  iO 

aooiosooi'-oaoaiio 

OS  CM  iO  OS  OS  »0 

OS  iO       OS  iO  OS 

1—1 

rH 

1-1 

r-liH 

1-1 

1-1              "■"' 

o  p. 
fe  © 

.CM    . 

Boooo  °,£'^  °  ° 


O  C3  o  <=>  •  O 

ftfl  Oft  •  o 

©   03  fe  ©  •  fe 

Uri  •*   W)  .  >> 


-°ft 


CJ[)  . 


pq  :  :  :  :m 

pq  :  :  :  :  :Moq  :  :M 

paraWpo   :M 

pqM 

pqMpq 

<N        O     CO 
O0        t^     CO 

O-^TPiCiO     io     to     o 
OS  CO  CO  co  (^     t^     t-  os     OS 

CO     CO     CO     CO 

r-    i^    oo    oo 

00 

o 

OO     lO 

o    o 

LO      >-0 

o    o 


2  2 

s  3 

o  o 

o  o 


^  00  CO  i-H     OS  ^  i-l 

■"^'-'oo  6    66  6 

6  dofcfc  55  5?!z;  J5 

SS  3  22  2 


^         T)  "3  T3 


3  "5"3  .££.5?  .£f  ,£f.£f  .£? 

OOO^icP      CD      0903      09 

OOOh-li-q  ^  tiA  A 


6    6  n 
X  &    6    6 

*  >;^  » 

M     M     ^    3 

'e   '3    o    o 
^   h-1   O  O 


55  55 
2"  2" 

3  3 

o    o 

o  o 


a  p  p  p  p  p 

ca  <a  cccccctc 

©  09  09  ©  ©  09 

P4  «  PhPhPhPh 


P    P 

09      © 

O    O 


.OOoo 

g  g  g  g2  !p  22  2 

OODOO  o  00  o 


0000 
2  2  2  2 
0000 


o    o 

2  2 
o  o 


OSO-HNM      SB      -j 
i-H  <N  tN  CM  tN     CN     tN 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


361 


©  g 

si  ii 


00    c3 


OOO 


CNOOCN 
00  to  rr< 
r~  io  io 


OOC5 


03  03 


§SS3S 


or  ..- 
y.  - 
lo  lo 


co  Xj  oo 

X  i~  -r 

t-  LO  LO 


(OOiflOl 


J  N  N  t^  O  ^f  LO  ffl  -J(  00  (D  t^  H  LO  Ol  l^  C  O  T  N  O  X  "  c  -^  -o  O  f  H  io  O  lO  O  O  «  O  O)  N  ffi  m  H  o  00 

'OlOWC:    X   —    r-0   ~  —  i  -  >-.  TsOKCTtOOO'J'KC'J  05  si  ~  '_:  ~  ~ ■  —  —  ~  'S.  -r  — ■■  lo  CD  O  Si  SI  O  O* 

^■^OcOCOCO^rHCOi^COCOCOCO^^COCOCO^OCOCO'^CO'^OOTrC^T-HeO'^OOCOCO^O 


tCSO! 


(O(DC>000C0O©iOrH(OCNTf 
LOOfflHCOOHOOMON 
1<OOOCNCOH(NCO'*00'H<N 


^  r.  lo  -h  k  c  c  -,:  x  Tji  in  O)  < 

—   —   CO  — i  0-0'  O  -f  C  O  LO  w  CO  < 
MHMHHHHOOHHH< 


I^JTPCOOHOOLOOONrtHCOrtLO©' 
'NOOMCOOlOCOHOW'^W'^OO' 
I^OOlHCOHOfCCHMCOrHM^'^rttH. 


io»mo««!OiNOx«oaLOM/jOw-.cciOL:io/cocovLOLOio(Ni 


CI  LOOS  lO 


lOjOOOhNOOOi 

CT>coiot~oo>or^i> 


CI  CO  lO  C-  00  lo  00  lO  lo  O  lo  lo  lO  i  CD  lo  OiODNiON 


OOOOIiOOlOOlOlonOONi 
N  ifl  lO  00  LO  T  CO  O  f  ffl  0>  (D  LO  t)<  [ 
■-     LOiOSlCOiCCDt^cOOOCl' 


>  Tt>  r~  <n  _( 

>  1— 1 1— 1 I-~  Tfl 
1  CD  CD  IOCS 


O  cj'o      '  P?  O      '  IT'O  03  o 
bJD_S  Is  cu  O  l>  <»  ° 


r>  o  P>  o  o  o  o 


,_,  j  d  o  ^'^ 
O  O  O  O  O  &S   O' 


wpQJ2^!§5^aMeQ5^aSa5Si25  :5555SwpQS3a5  :«<Mg£sm 


*-i      r^tN 


1  CD     CD        CD     LO 


o 

o 

c 

o 

s 

o 

ft 

ft 

ft 

ft 

fc 

ft 

„ 

>> 

t>> 

>> 

>> 

>d 

■d 

s 

2 

,C 

2 

H 

Wl 

bfl 

too 

b£ 

c 

o 

© 

O 

O 

A 

hh* 

h3 

1-3 

«l 

< 

►3 

Eh 

Eh 

tri 

!  o    ;      ;  6 

•ft     t-        CO     ft 


o  o 
ftZ 


^ft 


^  ©  _g  .s  ° 

©h^  "3  "3  hh1 

©     .  -S  .3 

CEh  Q  O  Eh 


ft  £     -s     s-e      -a 


c>C  tab 
'S'S 


£    ftftd 


£** 


o  •    o        o        o  o         o 


co  2    ©      ©2 
O     OO   O     O   O 


OO 


OOC 


CO  ^  LO 


^ 


362 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siaij^q— lonpoad  ^pui 


•ijaaj— ifldap  pnoj, 


•jaaj— mdap  po 


•}88J— 8UB{d 

xnnjBp  aAoqu  aprvjpjv 


•^88J— I8A8I 

eas    A\ojaq   apmi^v 


pa^nauad  ssaujpiqj, 


•^aaj— do^  o%  qidaa; 


^S'o  >  2. 


:  a 


6O10  60 

.3  ^.g 


c3  c3  s-i  c3  t-i 

OOOOQ 


Oi  O  N  l>  ■*  to  ■* 


CO  'O  CO  »o  CO  CO 


■V  i-l  l!5  00  O  (N  CO 


OhiOOMNW        h©NO 

acoHONcq  co  co  co  i- 


CO  CO  CO  l~  CN  CO 


o'o  o  w  , 

9<  P  »  9  P  ^ 


60  ^   60  rt   P  ©-.2         bO    •  !>   60  J>      . 

fq M pq pq E4 F-t S    pq  :^JgM 


iOO  o 

22£ 


P     ".CO 


UJiOiOiO 


IO  io  io  lO 


OOOOOO 


i-H  OS  O  O  OS 

IO  o  o  o  o 


ooiowio 

CO  -tfi  CO  CO  CO 
OS  >C  «5  iO  IO 


2s 

ft  o 

60p 

T3-^  o  o  o 
'£  •«  ^  T3  X3 

pSw  :  :  : 


8  £ 


M<*U5NOlflHlN 
OHOlOOMON 
tOcCCTtiOVM 


C*HOH^OH 


5<   ■  CO  CO  OS  O  CO  T 
CN   .  -<*i  CO  CO  CN  CO  CO 


CO  CO  >C  T  i-O  >C  OS  00 
CO  <N  rt<  CO  f  <M  IO  CO 
iO  OS  lo  io  iO  05  IO  CO 


«P5« 


O  o      ' 
ft  O  J 

©  t>  > 
bop  © 

who! 

!-,;rl  -~ 


lOiOSCCB     O     wlc        o 


0>    O 


©    ©  ©"3  § 

.C    .£3.3  0  3 


*  £ 


o  o 


.t3C3 


a  a" 

a  s 

©  o 

pq  pq 


£  ££, 


o  o  o 

a- a  a-:  *:  ^-:  * 

22Soooo  o 

©  o  o  tT   sS   «-T  tT  «-T 

rj^rj*        ©        ©©  © 

«««£  a  gg  a 

ddd£  £  ££  Z 


ft  • 

C?0 


33  o 


a   a 


o  o 

o        o 


Ifc 


o    o    o  o 

o  o  oo 

60     60     60  60 

Srtflrt-S  .3  SB 

_     ©©©©q    s    ■„  c 

60     60     60  60  60  60cfl     «3     CG  CG 

-4  -4  <l^<-<-©    ©    «  © 

■©    *©    '©'©'©'©  03^3     04  53 

.Sec    o    ooog    §    §g§|"g   -g   ^-g 

OOP  O  OOOQ  O  QOQOo  c  OO 

cOt^OO     05     Ohh«     CO     ^iOcOI>"X     Ol     O  <— I 


I 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


363 


4- 

a 

c 
c 

w 
0 

"3 
1 

j 

■r  ,C 
&  g! 

© 

•2 
o 

lO 

c/T 

03 

O 

Quit  in  sand 

Gas,  1,542  feet 

Gas,  1,526  feet 

Gas,  1,545  feet 

<2 
o 

LO 
LO 

m 
03 

O 

o 

© 

f. 

-d 
PI 
d 

t-l 

© 

'3 

w 

S8£ 

NhO 

o 

s§ 

cm-* 

m  o 

<M 

o 

3S 

oo  m 

CO 

o 

o 

CC 

co 

o 
c 

CN  ■*       .00 
OO      iOS 

r-  co    •  »o 

c 

EC 

O00 
LO  LQ 

IQ  m 

CO  O 

cq 

!C 

CO 

CC 

1,629 
1,564 
1,550 
1,560 

<35  t- 

mm 

LOr-c 

5 

00 

CO 

m 

o 

00 

CM 

CO 

[  - 

oc 
CC 

LO 

!C 
IT 

c 
— 

s 

— 

:~ 

iO  CO  oc 
—   71  — 

m  lo  m 

1,551 

1,553 

945 

1,537 

i-O  t- 

03  lo  too  00  t^  CO  t- 
00C2COlOlOi-HcOC 
t^OO02OOLOO}LOCC 

r—  t^  m  cn  co 


cococoOcoOcoo 


iOINtOCONcNrt(NMt-TCOmroNMOiOMtpi<CiC<5^00H(NHOINrtcoCNt<5 

X    C    V.   —    C    •_:    ~    ~    —  —   /■*r01«OMOHOrtO5>0)O'OHt»OO00NU5«!OHOCC0:'>Cl^CO 

',MC5'*mcOCOWoncOCOf<3Mmv*'«,OWC001'!fMCOHO^INNHOOO^OMCOC3>'*«l 


-tfi  r-H  LO  r-H  O  CO  <M  l>-         MC0L0'30Tf'BH*O*tl-/.XC:XiNC(0NNHroNHONTI<(D^Nt0Nl900CR'*0001N00 

O  O  O  00  O  00  O  00         ©  C  H'O  O  W  O  O  O  LO  h  O  C  O  C  »  3  /   ~  0C   O  O  O  Gl  -P  0">  CM  C-  CC  >— i  I f  — <  CO  "/  ff-  !C  O  *  N  Ol 

r-Hr-Hr-lTPr-ITCHrH-tfl        ^OhhOhhhhu'3HhhhhhOOO'*hhl'50hhm^oNN»'*'*^0'*hhioO 


J^ONNUJffiiOcOOaO      •  TficOLOOOcOcOr^CNr- 
iHWHTfrtlNNIMONN      •  CO  <N  i-H  CM  i-H  LO  t-H  r-H  i-( 


i  r-~  co  ~r  i — r  oo  i^ 

CO  CO  i-H  <M  <M  rH  rH 


OOOOOTI'iO'Hgj         ul  LO  N  O  ^  CD  O  W  N  *  C  M  ^f  Tf  lO  t  o  ir;.  [^  O  C  N  ^  N  H  C  1^  i :   r.  I  -   —    3  LO  CM  O  H  CD  O  H  [Q 
CD  uo  t-  CM  -f  CN  ■*  CM       MMWOMNcO'*e»ft<DOi5HiOHMNWeOiO>*,*M»M©MMiO«000>CT'*inrtCDOOO 

locomoimojioo)      o^o«io^^u5ioo)^oo©^®"o^ocsio^csioiocDNaiiotoN^()o©o)ino>iocD© 


CO  LO 

OCNTUJHCDOOQIOO 
OOCdCdlOCJiLOCDCClLOCD 


£££ 


o'go'go 

ftoftoft 
©  Si  a>  ►>  © 


r-H  <N  CO--1CM 


T-H  CN 


^H^m^PQWHO 


oooooooogo 

O  O  O  O  O  O  ©  OftO 

.333333335 5m w^ww 


d-d^ 

o  o  o 

O  O  O 


rH  <N 


c  c 

c  c 


-  o 


r-H(N 
■^-C_^     M    CJTCj^fK^    c,    OCT- 


•t!  -d  x)  'C  -S  -o  "C  •«  .S  Sot'H  S  2  o'^d 


!  O  o 

ISi" 


o°o    • 
o  ft  o    • 

^  CD  fe  >> 


O    oo    r~       o    >-h    co 


CO  CO^CK      Tf 


z  K 


<  <  6 

f— (      rrH  <H 


003 


o    o 


50  e»3      ^,      C»  rH      C3S      CO  W 

•_'  x     ~     ^  •  *mN    h    « 

©  0000000 

z,  XX*  *  *  *  *  2°°   o   o 

s-T  C    C    M  M    M    ti  62  ^    ^       ^       - 

|<  §   §   S  S  .3  .S  .3  fl  rt  fl   fl   fl 

c  §   fl  .S  B  B  B  B  V%'%  '%  % 


6 

6 

6 

6 

6 

. 

S5 

^ 

fc 

» 

^ 

PI 

ri 

© 

© 

© 

© 

© 

C5 

O 

O 

O 

O 

P 

o    o 
S  IS 

o  o 


0 

O 

O 

O 

O 

O 

0 

a 

O 

O 

O 

CJ 

bfi 

be 

M 

M» 

60 

60 

PI 

a 

PI 

P 

PI 

- 

d 

a 

PI 

PI 

A 

a 

-- 

cd 

<S 

CC 

CC 

— 

© 

« 

^ 

tf 

Ph 

Ph 

« 

03 

rs 

c3 

C3 

c3 

01 

fl 

= 

PI 

PI 

PI 

c 

© 

O 

O 

U 

O 

CJ 

0 

lO     O     t^ 


0000 

CU       CU       CV           ©      ,FH  '^h  *^h      *^h      *-h  qj 

©     ©     ©       ©    ,CC,C    fC    -C  © 

aoo    000000  o 

00      Oi      O         t-H      (NCOTK      LO      CO  1^ 


364 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


X3 
T3 

fl 
o 

O 

I 

r< 
«0 

© 

o 

CO 

ss 

CD 

? 

o 

CO 
o 
IS 

CO 


CO 

CN 

oo 

C3 

a 

•H 

TO 

:S 

•S|8JJBq— ^onpojd  teiiini 

:S 

•^98j— md9p  \v%o& 

•CO 

CD  O  CN 

•599j— mdap  no 

"OCDtD 

HHH 

•}99j  — gne^d 

CT>  CO  ■* 

ran^p  aAoqB  gpnmiy 

•^89J— I8A9{ 

O  MO 

bos   Avojgq   epn^jy 

^rtrt- 

CNCNOO 

•%wi— 

COH 

9 

pg^Jigugd  ssampiqj. 

CD  O  CN 

•^88j— do;  oi  md8(i 

iO  CO  CO 

CQ 

rl  ,-(.-( 

CD 

rHC 

in 

a 

ri3T)Ti 

& 

o  o  o 

£££ 

££.£ 

WWW 

iL  <o  i    i    1  jj 

s  8  ®  P  S  o 

^< 

o 

& 

o 

eg 

^) 

1 

6 

fc 

fe 

bO 

CI 

g 

q 

(A 

§ 

o- 

a 

o 

o 

o 

o 

eg 

a 

a 

£ 

CO 
CD 

CJ 

P<^ 

Si  o 

S* 

g 

o    . 
33  o 

H 

r 

CO                        1 

CO 

© 

CD 
CJ 

CD 

e 
i-3 


■spjjBq— ptipoid  \b\%xii 


•;89j— qidap  xb;o  j, 


•;aaj— q^dap  no 


•}98j — auB^d 
umiBp  9AoqB  epnii^v 


•^99J— -[8A9] 

B9S    Avopq    epn^jy 


•^99J— 

p9^Bj;9U9d  ssgujprqj, 


199J— do%  o;  qidgci 


go©  dfl-s 
cH«2  co  >.o  © 


I 

ft  • 


0 

o    . 
33  © 


CO     Tti     -<J< 


£    m 


BLATCHLET] 


TABLES    OF   WELL   DATA. 


365 


QC5 


03  CO 


C3  W> 


ZTjO 


©  o 

II 

5<l 


££ 


|hhO 

lien- 
£§££03 
-u>  O +»  +j  s 


O  CO 


§2 


C<«eNt--COt^OCM-^< 

CM  ■<*<  t^  CO  <N  f  -  " 
OlOMCS     I   < 


CMtt  CO 


t»  M  iH  N  lt  ffl  M 
CO  OS  »0  CO  C5  ■*  CO 


'0C00- lOiO" 


t^r^t^-iOiO        iftOOOMN 


oooocoi^t-^ooocot^ 

iO  W  H  iO  lO  t  i-l  M  1< 


iOOCOOOO 
t~-  OS  CM  iO  w*  t~ 

llflffiHlOOH 


SitDtOONINOOiOiOO 


CM  CO  CO  ^ 


100OOOO' 


hn      eo< 


ooimoocwtoN 

OPJlflOOOlONOO 


'  O  O  CO  o  o  o 

»  i-H  CO  O  O  O  CM 


ooooor-< 


OCOCOcOOlCOiOOlCOiOtD 


00  CO  CO  00  00  CJi 


OSoO      .   O   o 

aa  o  ft  •  fto 


°  s 

O  ft 


■o    fe  s^ 


o  ft 

fed)     •  >  ©     •  fa. 


s*  w  >rt  .  u  flirt  S-.  rt'rt'rj 
O  03  5  .  O  C3  5  O  03  5^ 
ftPl   0,-ftfloftPlOO 


S^g  j>?o 

ftfl   O^  ft 
CD  c3  !*  o  ® 


!"uiri 

■  go 

.    <  fto 

t-TJ.S'rt  £.5 

02  :W  :m^ 


o  o 

££ 

'd-d 
o  o 
o  o 

5  5 


a.    ^ 


o  o 

©  © 

c3"rt 


&6h 


6  6 

££ 

a"  a 

c3  e3 

o  o 
o  o 

PmPh 


3     a 


o  o 


oo    o 


o  o 
©O 

©  SP 

q.9 
1-1  o 

o         ll-S 

o       a    J 


■fl.fi 

OO 


366 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


SS.S 


•si9JiBq— jonpcud  leprai 


•%ddi— qjdap  1^03, 


•198j— mdap  \\Q 


•;aaj — atrejd 
run^p  8AoqB  apniptv 


•^88J— \ZA9\ 

■eas    A\opq    optvjruv 


pa^j^uad  ssau^oiqj, 


•^88j— do%  o%  mdza 


S£ 


o    . 
13  o 


O  O  O  O  iC  o 
2'/!O00  CNkCO 


i-  iO  — I  t POO 

-H  CO  CO  >o  CO  l> 


X  to  X 

ooj>o 


o  io  *  io  o  w 

NTfNNOO) 

>a  io  o  (o  to  ic 


*  J;  Cj  JJ  Ci  ?i 


OtONINCBCR 
rH  ©  t^  W5  JH  M 


OtO»CiOiO 


f  ONtOCOOilNrt 
ONCOCCN-ifTjit-, 

ooooooo-* 


s§ 


toiOMNioiwNoiiHoortNairHMN^Hocioaia! 

—  WCOCOCOOt>iO»0'-OCOCOlOcO>-OC'OCOr^OC<— ICOCC-* 


■OOtO'fNHOOcS 


irtiiOh-COiONOOrtCSfJOJOO^aiNXOsaNiOHOi 
iMtOfOCOCOOtTfTtitOMTrc^^otOINHOOtOMfO 
'00O'3"^iO>-HTtiOOoOO-<»<OOO>-i>-iOOOi0 

,_r      i-Ti-T   ,-?,_;' .-r.-r.-r  ^-rrH,T-Tr-r»-?^ri-r^-rr-r 


OOOOMOtOMOiH 
OOOC'OSOIOSOJOJ'O 


iflOHOWOOOiSMaNfMOONiOOONMXOOli 
MOMfWHOSMHNfH'NNHMNOOtDiOHi 

oi  co  >o  o  a  >o  io  oi  >o  io  >o  io  m  O)  >fl  "3  io  <o  co  >fl  io  m 


^^^    •  T1  ^  T*  ^ +j  T*  ^    • 

13x3  J='Ot3i3'C)t3  J-TJ'CJ'd 


oosooooojooo 
afloft  •ooaoooooftooo 


^  o 

■n-d- 

cq    : 


O        ftfl   O  Ph    •OOP<OOOOOP<00 

i  -d  £    «  §  .£  •£  t3  £  £  -c  £  .is  £  a  £  ■£  .is  £  £  -d  d 


■8tj 

o  o 


•d-d.; 


:W^ 


•*J<        iO  K5     •f     '^l  ' 


ao  t--    oo      t-    a> 


'  co  io    oo 
l  oo  oo    oo 


CO  ■**  lO  t~  CO  Q>     00 

6  6  6  6  6  6    6 

ssaass  a~ 


o  o  o  o  o  o     o 
o  o  o  o  o  o    o 

Q-i  Ph  Ph  Pli  PU  Put    Ph 


IN     to     iO< 


o  o  o  o 


o  o  o  o  o  g 

.,  .,  -,  »  -  o 

CD  CD  CD  CD  CD  O 

O  O  O  OO  ° 

CO  o  o  o  ■ 


55  5?  5?  p«PhPhQ<!z;  55 

„  o  o  o  o    .,  ^ 

CD      CD      CD  OOOOCD  CD 

g  g  S oooog  s 

o  o  o  .vw  o  o 


9  2  2  2  2-2 
222222  3 
oooooo  o 


pq 


o  o  _o  o^o  o 

22  2  32  2 
oo  o  oo  o 


o  o  o  o_o  #- 

2  2  2  23222  2 
o  o  o  ooooo  c 


<  Li  to  N  00  o  o 


i— i   HtN  n  ^fio  o  n  »  o  ohnm«  is 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


367 


•  .2   ~ 

o3rt  P 
OT  c/T+f 

!50cq 


-<> 


+a  ° 


Mi 


C3   O    53 


«2-J<£ 
^8- 


©Vo 

©^ 

5-1  co 
O  C3 

550 


>2  <2 

OiO 

c3  dWo 

llll 


ft 


p    p 


co  oi  CA 


—  >-  ■ 


«MO^O!OCOrt     I    <£>  CO 


i  CN  r^  i-O  CM  t^  CO 


C-J  rH  O  O  N  i- 

OCC13-- 


§8! 


1<HH-ONCqHi)(NO- 


OOOOi 


—  uo  re 
O  ^  OJ 
l-7  O  >— i 


X  o 


2N      £\ 


3g 

o  SO 


t^  iO  SO  SO  lO 


iSO^COlM  i-~ 


co  so      u-t  tj.  io 


33S 

O  u-  so 


'-  C:  Sj 


5 

► 

M  : 


:mt 


2<P£ 

sfus 

cqcaWS 


C3  o 

■s-a 

pqW 


ftss-  'o 


o  o 

O  ft 

fe  (to 


°  2 


o    •  o  o  o 
O  k"  o  o  o  . 

5  EH  5  W  5  Eh 


SO  SO      -*ti 


CO      CO      CO      CO 


i-o      co    so    t- 

CO         CO      CO      CO 


o 


<N^    Q 

o 

•-H 

►2  <° 

d  d55 

55 

o 
55 

-§« 

C/j    VI    fe£) 

E3) 

c  oO 

O 

-iJ  x 

c-a-h,' 

— 

X 

<M 

o 

o 

o  c  o 

6 

o 

55 

52 

52 

£££ 

k. 

E 

0 

o 

C3 

c3 

o  o  o 
cS  cS  c3 

T3 

T3 

'3'O'C 

■C 

G 

C3 

C3 

C3   C3  C3 

X 

(3 

M 

H 

www 

■A    ~*  & 


^  &  a 


o    o 
55  55 


60  P    fe. 


■O"         N     N      - 

6      6    6c 
15     55   £   fc 


CO     CC     OJ 


°    5 

55     55 


.2.2    .2.2.2  .° 

coo  o 


OO 


C3   C3  C3 


i-<  oi  co- 


OOP 


c  .2    2  .2 

3  3  3  3 

o  o  o  o 


c    c    c 

3  3  3 
o  o  o 


— i        <N        CO     "^ 


368 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spjxBq— pnpoid  itji^tui 


•jooj— mdsp  pnoj, 


laaj— qadsp  UO 


•^oaj— Qwe\d 
umjep  9AoqB  epnimy 


"488J— \QA9\ 


pa^j^angd  ssauspiqj, 


•}9a;— do;  01  mdoa 


fa  oi  C3  ato 

CO  .2^  >  O,© 


S£ 


23  o 
02 


05   <» 

JT'  '/J 


o£ 


CO  -H  Tt<  i-H  CO 


uNOJ^H 


I  CO  CM  CM  00  ^H  CO  C 


iflOMOO  NffiOOOKJOM 
OO^^r-lO  -*1  f-  O  00  CO  00  t—  TP 
OS  'f  lO  00  O        HlOO*lOClCOlO 


*tf  c3^' 


!t3  O 

cqcoWcq  : 


:  o3  (=1 


fa.flT5  fa     -T3  fa  Qt3 
ftrt  Oft    'OftflO 

oq     W(S«23wm5 


OO^ 

coH 


c3  i-i 

OQ 


i  tO  CO  »C  iO  o 


OiOCSiOiOO 
t-  t~-  C3>  CO  >0  t>- 


C'C'tf  S-fa£ 

pq  :  :mMtc 


2S2 

CO  •fl*  CO 


82£ 

CO  "3  CO 


(-1    c$ 


c 

c 

c 

^~ 

fe 

£ 

£ 

1? 

^ooo 

5 

•d 

o 

T5 
O 

O 

o 

o 

o 

o 

* 
£ 

41 

* 

^ 

^  05  ©  CD 

M 

M 

M 

M 

3233 

a 

s 

a 

S 

££££ 

o 

O 

fc 

fe 

d 

fi 

o 

C 

M 

ts 

9 

B 

fl 

jq 

o 

o 

MWpqW 

<B  4)  »  » 
*C  TJ  "tf  'O 


3 

3 

3 

3 

o  o  o  o 

rf  a  a  a 

O 
Pi 

3 

3 

o 

o 

o 

o 

toco  coco 

GO 

o 

o 

CO 

■V 

IO 

<N 

CN 

CO 

T 

BLATCHLET] 


TABLES    OF    WELL   DATA. 


369 


o  9 


oz 


£«3 

O  ©  li 


*2 


£2 

Oco 
CO 


COCO       CO  CC!h3 


2  >> 
A 


O  O  ce 

38K 


2§ 


r~cot^co-^<r^r^r^i^ioco-«coc2-HceL'::oi 
0»NWO00«>0«H00ONXONXwwi 

Oico-^,cO'-iO"icO'^<coi-i'<fcoi-i'<r'cO'-e3<cO' 


LOO        NiOOCNiOO        ONW 
O  CO        CO  t>  (M  "<J<  CO  th        CO  00  ^H 

ico     t~- oo  i-i  r-i  ■<*<  ic      oo  oo  i-t 


co  t^  co  oc  co  ce  co  : 


)lOr-O500>-(O5I>lC-,3'CO 


Od«CSrtrtO"O0C^M 

Oiotoommtoooocieo 


O'«lOL-?;CCSCNL';N£aM.0MNrt 
•*  -h  o  CO  i-O  —  X  O  N  >C  CO  -h  lo  CO  -h  uo  CO  CM  CO 
CT>  CO  iO  CO  t-«  OJ  CO  uo  CO  t^  uO  -X  t--  LO  CO  t-  u? CO  t— 


©  ■<*  O  kg  lOOOi 


_  OC  lO  CO 
COlOCOCO-^t"9<COOCi-l'*iCO 
idOlHWl^OlONiOCON 


rtCOlfllOO!©         00  00*0 


H   fir 
O  c3 


<>0  C3  o 

^  &a  o 


-r  _ 


~1 


S  £3  I  &I 


s  a 

P5CQ 


•a  2  o-n  5-s.  2^-a  2  «.a  go.S  So 


^  o 
.ax) 

a  : 


55    i'gS 

o  a    •  O  ft 


C3   5 

a  c 
2? 


Wps^Wpq  :  '.pcWehS    oaco 


r^ 

oo 

oioowc 

.- 

05                                   IT 

C 

"5 

t 

■* 

■<J<   -"*<  tl   "*f   Tf 

"* 

■* 

• 

co' 

CO 

LQHHH' 

o 

o 

C 

CO 

£ 

z 

o 

c 

o 

6  6  6  6<^ 

I- 

0" 

c 

c 

fc 

2 

ft 

ZZZ^c 

c 

c 

c 

-g 

"3 

£ 

z 

o 

- 

o 

'0'd'*0''rt'Z 

fc 

2 

2 

o 

o 

p 

E 

o 

C 

o 

O  O   O  o  P 

= 

= 

£ 

p 

^ 

M 

PS 

s 

£ 

c 

C 

c 

•a 

.a 

f- 

a 

a 

*j 

f 

^ 

a 

5 

i 

M 

M 

0 

o 

M 

* 

M 

mm3m& 

- 
- 

M 
£ 

£ 
d 

» 

OT 

c 

« 

pj 

M 

tftftfFH^ 

c 
% 

C 

3 

X! 
O 

a     afta&&    g< 

|    lla-IS    S 
13    13  (5 13  £  m    £ 


—24  G 


370 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES.    Tbull.  no.  22 


■siaxreq— ^onpoid  im^mi 


•;89j— q^dgp  pnoj, 


199j— qidgp  no 


xnni'Bp  9AoqB  gpn^tuy 


-}99J— I9A9J 

B9S    Avojgq   gptni^iv 


199J— 

pajBjjgngd  ssgujpiqj, 


199J— do;  oj  qidaa 


9  ©  <g  c3  pj"5 


a 

2* 
w 


r88 


??§ 


OOOOOHOOWI 


iOOONOIO" 


iQOO(MO>OOt^OO 

OOOONffflOOOM 


c3  O 

a  o 


'CO  3 


o  o 

O  O' 

mm 


-5  >> 

a  es 

Sec 


3  C3 


OOVlOMiOlOOMO>OINM!OiOONO")0 

nMsanto^mMooowTtioNOTjioio 


>o«5io>-Hioo>ofooooa5i^'<*< 

)C5         OINHH'*®         (Mi-HrH 


SOVjOtOOOiCMOONOOHiflONOOifl 
:(DNNcOONlOOXMNlONMOCONlOa 
DOJ'HCOiOt-OOOiOiHCOlOlOt^OicO'ONlON 


a  o  a 
cq  :ggpQMpQ  :  :  iroccMMSwrnMSMS 


B^t?  kL"S  Bts  J-d  J 

sJISlllllgf  8 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


371 


03  03 


<N  as 


<2«2 

05CO 


4?  2 


CO  © 
oc"e8 


Is 


o  m  o  oo  i-H  oo  co  i-iio  oo  co  oo  -*i  o  o  m  o  m  co      o  oo  tti 
©©MHOffitoNOcoMOoioociiOMcoH      in  co  >-i 


ooin      ioo>oiaHM«ioooa«)»ioMot>NoooN 

OO^m        C0Nt-(OO5iO00«5-HNOsmtNCO00O5«IN(»tOMh- 
hOO       NCONrtOXOMHiOHi-iiOMi-iMMHHOltOCOH 


oom 
co-^m 


lOOiOmOlNMOOONNMiOCOiCMMOOO 
(OCONMO^HCOOMOONfOiHOCONNI'IN 

t^.-KNcomoo.-icocicocooi<-icort.-icocoinoOT-i 


i  cc*1  in  oo. 


"OOMHOHMH         MIOM 

m  co  oo  en  i-h  .-h  co      as  >-i  co 


iMOOl 


omom<N>2©<MineN)t^i--— immom 

!OHij<l>0)OflMOi0001<TiioocO(D(0 

CT>coini>ooocoino5inmo500cNcoin 


o  >n  o    •  o  o  m  o 


momminooco'-HOoooocooooocoooooo 

Ot»CON*NU)NCOt"*0'-lNl0^tOHiONW>0 

cNincor-oiiMinc^'^'t^o-Tticor^inint^oooicNint^ 


mo<N      m  t^^H 
—  Oi  t^      t~-  Oi  oo 

in  i>      co  m  t>- 


H      tf 


.        o      o 

«     .2    .S 
8      ►    P 


m    pa 


ft 

^j 

60 

60 

60 

> 

ft 

«5 

■^ 

-< 

w 

a 

- 

_,- 

T 

■S 

60 

0 

a 

CI 

a 

n 

s 

9 

H     £ 

fc     £ 


372 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spuBq— jonpoad  fei^ni 


•188j— mdap  i^oj. 


•;88j— mdap  no 


189J— 9ITBld 

umjcp  OAoqB  8pn;i^iy 


p8^BJi8U8d  ssau^oiqx 


•;88j— do^  oj  mdacE 


B 
a 

ft  • 

§  . 


2dS 

03  ON 

=§3  8 

rOCQO 


t-    l~    <D 

.2.2  3 

111 

c3  03^ 


H(OteNiOiOiOiOO«500r/  iCif 


U5NNOO' 


iiomoortioi 


lOiowmoioooNioiO! 

'N(CNMiOOK)«DMO-»,( 
i1>>*lflNOOHHHMir,OCi 


'S^SSjS 


^O'COOiqio      MNOioioooioicoonooooicoio'ot-Oi 

•^    y    CiOI-O^I         fM^OOOCOMMN-^^NCDOtCNOC'TtiXCBfC^i 

io  c  i-  o  n  lo  o     ci'oaoNiooj'OOJioiONxoiOi'-iNmioiONOii 


1     •_&  2  &  <=> 

o  J72  fta  o 

A  got  d-*d 


O  o  © 
fto  & 

©  te  " 

bfl  ^ 


-d  £d  j-'d 
w  o  ©  o  °  o 
fl  o  fto  fto 
©  t>  ©  I 


*££,£ 


w   >   w      *    w   ■>   ^    &-   ^f    (^      •  w      ■      ■      ■ 

•d^-o  cg^d^d^o-dooo 
'C  •-"  'C  d  3  -Jh  °n  •-<  'G  •-<  "d  '£  "d  *d  'd 

cq^cq  :cQMm^m^  :«  :  :  : 


|<N  CO 

•dd 
i  o  o 
i  o  o 


JIM 

oC3^ 


00  T-l 


°    1      8 
.9*  .9     3 


6  & 
a   § 

©  tu 

fisa 
© 

S  P5 


ft       ft    ft 
©        ©     © 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


373 


©  © 

"eats 


o  o 


i  o  t~- 

iCNcO 


■>    CO    CO 

3  03  c3 

SCO 


T2  ©  © 

-js  §  *  * 

CO  C^    ^  •*-=•  -4-3 


,5  © 

02 


'-.« 


®  5 

©  eS 

■5J 


II' 

.S.JH 

CO  CO 


(NcoiC* 
lO  CO  t^-  iO 


OOiM 
lO  >o  lO 


as  o  cr- 

CO    Tl*    T-t 

r-uo  uo 


co  -v  co 
to  CO  t~ 


lO  lO       »o 


rtG;0rtrtrtNT)iN00O 
CO0C— H3O0COOO00N 


i^  t—  i^  cn  i,  i  -  cn  i -  cn  co  cc  co 

l>  "O  t—  CO   s    ~1  ~    S   ~S-   ~  O  C*- 

"OCOLOCOOcO-^CN^HCOOCO 


OiciOio  or  co  io  o  r~  t^  i. 

OiON-taot^oOHi 

Olt^-^CO^COOCOTTiCOi 


CtDrf  CO'OJ       ■*  rfi  • 


OO^CfcCnOSGOcOOOCNO 

CO^HOO'*fCft*-<COC!iO-HCO 

MiSiOMONMOOOiH 


COCOCOOOCOCOOCCOr-Ht^Tf-^ 
CN-rCNCO— <t~C5  —  — "OOO 

0>H0)tHl000O««iHl0rt 


lOWiOiONNiOOCOWI^ 

odiNoccoNc;-/:- 
lOt'OHecH^aoi-iM 


00  00  rt  lO  in        CO  CN  CO 

or  >— i  o  — h  cn      c.  ~.  x 

<#»Ohe5       COO 


OOCOOOOINCOOO 

r^io>— laocoiOcocN^-fio 


OOOiOOOiOOOOTFTj<-*f< 

lOt^iOCO^OCN-^COCOCNcO 
M»OMiOO!C0lOCONlO6iO 


LO  lO  00  N  lO       co  -*  oo 
"i -*r  r-* -*r  t       — iCNCN 

35  CN  lO  lO  CJ         10K5U5 


OOOOt^NOiOC 
-tiCO^iCNCOCOCOCOl 
©NuOCOMnoOCCi 


CN  CO 


O  O  O  C3 

©  ©  ©  cS 
SXJSjOSjO^ 


o 


-d-Cd' 


:~" 


fta 

©   C3 


fa  * 


ft  fl  o    ■  -^  o  ft   ■  o 

CO  CO  M  Eh  S  M  PQ  w  W  H  § 


flfiooft 

©  c3  fe   te:  © 

pspaWWpa 


X  o  o 

.fa-OT3 

W  :  : 


NOW 

CN      CO      CO 


c 
7 

CN 

c 

c 

i-H      CN 

6    c 

1-H       CO 
6        C 

c 

2 

c 

c 

c 

y 

c 

c 

IC 

cc 

— 

M 

CN 

c 

CO 

c 

7 

i 

OSS 


O      O 
CO      co 

©     © 


CO        CO        CO  CO 


z 

0 

rt 

a 

0 

o 

o 

IS 

ES 

CO 

co 

Ph 

3 

3 

S 

^ 

u 

CJ 

CJ 

G 

O 

o  o 

o 

fc 

^^ 

55 

CO 

222 

CO 

©  © 

tX) 

tJO  so 

Si 

O 

o  o 

a 

« 

PStf 

PS 

So    OO 
o        .    . 

PS     « 


a 

£ 

£ 

a 

s 

g 

g^^  H   W   W   W   W 

II  ^  -i  4  4  £ 

S-c  B  3  3  3  3 

mca  m  a  m  m  w 

©O     H     IN     M     *     U3 


p 

1 

1 

1 

1 

.2 

■O    O   O 


t- 

E 

3S 

5 

g 

^^3 

- 

mvi 

OD 

CC 

oo 

C 

374 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


'sjaxreq— ;onpoid  i^ui 


•188J— qidap  ibjo  j, 


•188J— q^dap  no 


ran}i3p  8AoqB  apnitqy 


•}88J— \QAd\ 

■B9S   Avopq   apniniv 


pa^Jieuad  sseu^oiqjj 


•}8aj— do}  oa  q^daci 


i  CD    i     i      I    .J 

g  o  «  c«  a© 
02 .5  <»  >.2.2 


COiO 


©mirjiot* 


ooooo 
oo  c©  o  co  o 


^W£ 


co  t-    •  cn»  o 


8  :§ 


OOOOO 
CO  t-  CO  CO 
U5MOIO 


t>-^MiTtiTri-^to^,-^^Hrji-qieO'— icooocc^i 


IIOOHMHOi 


MMiO»tO!D000100tO(DNHC1tOtO«5HHCDHOOHtDriiOiO«0>(Min 
(ONNCOOlOHOOoOMOONHtHOHaiTtiffiiSNMOOMtffltficOceO 
NOOOOOOOOOMOOHMHeoOOMVNHWiOOOHWOOOOON 


OON"5|O00OON00HOi0*u3OOOU5i0OinW«)Oi00>l»OOWffi 
•*lOMHMCN'*rHHtO'-IO'!t,NTI<T)<lt:coNcN|COlOt^(NCOlOCDHCNOi-ICO 
NiOiO>OiOiONu5iON«3iOiOMOO«iON05NiONOiN>Ot^iOiO«iiOO 


6    6  6  6  6    6 

®  .s'.sT.s.sf  -2 

'p,    PtftPnft    ft 

©  ,2,2,2,2  ,2 

3  3333  3 


<nt)i'  oo  co 

.2  6  6  6  6 

ft  ££  £  £ 

•a  >;^  £  >; 

«^h  c3  03  c3  C3 

.  OO  O  O 

^  02*02  02  02* 


1  "^       5 

6       6  6     ^1 
fc      ££     g 


02*02"    o 


0     OOOO    _o 

3  3333  3 
0  0000  0 

Ohio. 

Ohio. 
Ohio. 

0 
3 
0 

0 

3 
0 

0 
3 
0 

0 
3 
0 

0 

3 
0 

0  0 

33 
00 

0 

3 
0 

lO     (ON00O5      O 

~H      1-H(N 

co 

"* 

0 

CO 

r- 

000 

0 

155 

S£ 


•rt  o 
02 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


375 


£    -co 


<m 


03  >  03 

o    o 


"ft3 
Ow 


o"c3 


m   »   Ol 


c^i  io»oio 


lONiOiOMifliOiO 


OONiOOON        lO  O  O 

offlWHOOn 


coooo 


-"i-t      oo  co  oi  t-  co  i-i 


OtXNffl. 


CONHtO 


SI 


lO  lO  LO  00  CO  < 


is  gas 


00OOO00H00OO        HrtOOMHOH 


M00M1O 


328! 


!D  O  l<3©  ' 


LOOOOC6         O  CO 


<N  1-H  1-H 


NHN^NN       tj>io 


iOOOO>0  00       OONO 


O  N  O  O  iO  h        idHLlOiOe        O  O  iO  O  <M  O        VCOOOOOhnOOO        OMiOOOOHiO 

i-h  cm  co  cxi  .-I  to      o  f  «  «  Tf  io      oioiNMiot-      C3  t-i  co  -h  co  t*  ct>  <m  i-h      o^oeiNCMia 

lOiOOllMiON        HiOONiOt^        NiOO>NlON        CNHOiOlO<N»OCNIioiO        lONifl  •*  NO  ifl  IO 


o^  ftd  o 
•S3  o  C  d-~! 

WSmmW 


fcL-d   • 

o-d  'O 

SM  : 


:^ofl 


-,  ^  .2  60  " 

3 .s  o'sn 


O  °  03 

o  ftd 


C"3  ft 

-goS 


fcfd 


Jlifll 


OOOOSobO      • 

flooofloflo    • 

caWWWmWmW  : 


.J* 

03O 


..d-d  d 

S^  :m 


C3   O 

a  o 

*£  . 

o-g^  o  o 


d-d -a 


58 


(M  ^H  CM 


o  r- 


CM     CM  O  CXI  <M  ! 

CM      CM  COCOCO  ( 


o 

o  o 

Z 

££ 

a 

d  1=1 

o 

o  o 

f2 

on  xn 

C/3    1/3 

5 

O 

uu 

i-l  o         o 


o    oo    r~    vo 


o    o    o    o 
fc   £   55   £ 


CO  i-H 


55   fc       fc   Zcm 


o 

o  o 

o 

1-1 

T 

£ 

££ 

Z 

o 

o 

o 

o 

ft 

£ 

fc 

ft 

>> 

>>>> 

>> 

cs 

— 

C3  03 

t-i    tH 

t-i 

rCl 

.4 

fl 

ri 

O 

oo 

O 

a 

S 

1 

a 

co 

COCO 

w 

cc 

w 

CO 

w 

o 

o 

ffl 

© 

o 

S 

o 

<B  O  O  O  O  C 

ft 

ft 

ft 

ft 

ft 

ft 

ft 

ft^Z^^^. 

o 

1 

£ 

s 

3 

en 
3j 

</> 

ffi 

j§  n"fl  a  a  d! 

O 

'5 

3 

3 

3 

O 

O 

--  o  o  o  o  o 

-i 

h-i 

i-5 

i-4 

ft 

ft 

h4 

4ooooo 

>  > 

WW 


33 

mm 


o  o 
id  3 
OO 


.d      rd       rd       ^ 

O  O  O  O 


^d  ,d 
Q  O 


o  o  o  o  o  o  o 

id  id  id  id  3  3  id 

O  OOOOOO 

I^  MOIOHNCO 


W 


376 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siaxreq— jonpojd  i^xjux 


•aa9j— t^dap  ibjo^ 


•198J— Hldap  no 


•^aaj— etrejd 
mn^p  QAoqB  epn^piv 


'189J— [9AQ\ 


pa^nanad  ssan^otqj, 


•^88j— doj  01  mdaa 


g  o  ©  c3  g  © 
d2<2  ©  >  .2  © 


P<  • 

c3  O 


lOCNCNCNcOCOCNCOCOCO 


iO  CO  CO  <N  iO      •  (N  CN 


OOOOO 
,_<  t^  _l  _<  ,-! 


oioiooiom 

O  t^  (M  o  r~  CN 


lOCOCOCOCN        COCOCOCOCOCO 


(0  00O05H         10  10®IO>00 
-*00  050lO  fflCOOOHOH 

lOCNCNCOCN        (NNMCOMM 


CT>  1-1  Oi  CO  CN 
O  t-  r-CO"*t< 
t^  CO  CO  CO  co 


HOCMOO(N®iONHOC(OC)"nt»COO>OMOtO'*OHO!DH  lOHOHNOO 
NtO«5tOOOOOfO(NCOTf(N-*^MINLniOOOO)HNNIX)  t-H  O  CN  CN  CO  IO 
00  00  »0  00  ^H  00  00  00  »-H  i-t  00  00  00  00  00  00  00  00  00  00  ©  00  00  00  t>-        00t~O0O0O0O0 


lOOffllOCOOiOfflOMiOifl' 
)H-*«  rlrH  r-li-li-ICN' 


>o^oca>  _  _ 

'0«H  C75.0C  CO  "O  CO  t- 
iCOiOCOCNCNiOiOCNCN 


OOfflWiONOMNHNOOOOOMfOH  0*-KM^HOr~ 
TOOrtNOOOOOOININOOOONlC  OltDOOHOO 
I  CN  CO  CN  CN  CN  CN  CO  IO  CN  CN  CN  <N        CN  CN  CN  CO  CO  CO 


°.2 

cq  : 


O  c3 
P-fl 

-Sf<3 

TJ  cj  ' 

•C  a- 

cacat 


|  o  oM 

I'd  "3.3. 


!t3  « 
o  cs 

,  .►J  . 

'SOOOCOOOCO^oOOO 

m  ::::::::  :Spq  ::  : 


o  o  o  o 


CN        CN  -ti        00 


(NCOt~-COt^t>.CO^00     Tt<     -tfi  00  -f  O        >0  O  CO  ©  < 

co  co  co  co  co  tj<  io  co  co    co    co  io  ■*>  r-      j>r--m©< 


o  o 

o 

o  o 

££ 

£ 

££ 

0  s 

3 

ri-3 

o  o 

O  CU 

<Q3 

co 

C/3    Q) 

L 

03  03 

rt 

C3     . 

oo 

CJ 

OO 

,  ,-H  CO 

IO  ■>»»  CO  i-l  CN CT><  Tl  1-1  1-H  (OHP5S05H 

.       .       .       .  CO  CN  i— I  IO  "*<      CO  ....  

O    OOOO OOOO  OOOOOO 

S>        ©©©©S^SfSfSfSf    ?°    ©©©©  ©  ©  ©  ©  _ 

02     moQaQoQ.Sf.5f.Sf.Sf.5f  .SfoQoooQcc  wmaimuim 

o    doodooooo  o  iih4t4i-i  >4i4>4>4i4»j 


o  o 

22 
oo 


.1* 


oo   o 
OO  O 


^.o.c^o.o^o.o^o  o  .0.2,2.2 
232232332  2  2222 
ooooooooo  o  oooo 

M^iOtOt^XOOH     CN     i-HCNCO-* 


.2  2  2-2  2.2 
222222 
oooooo 

lOCONOOOO 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


377 


<S,Q 


©  ©  © 

£>£>   © 

co^oo 


PI 


V)  xr.  m 

03  c3  03 

oco 


2  ° 

03   © 


©  o  o 
©  ©  © 


CNtp 
in  o 

1-1  © 

V)  '-' 
03  O 

OZ 


—  73*-  T) 

co  ©om  © 

©,Q  SX2 
?—"««  — 

c3^  c3^ 
02       CO 


:S8 


COCOtN<N 


—    X  '-   /jtHIOM 


OtDWOOO-HO 

oocowc  to 


-HOCOtONt^ 


3      •OOCOCd'-HOC 

s_h_m  i-^  «<_■  <_<  u<j  i~-     icok  i--  r.  -  :: 

CCNMU5MNN      HO  LO  lO  in  ■*  lO  O 


)  COO  O  CO 

<  X  O  0C  f» 


tOOJtOQCO 
00(DlOHO 

eq  io  co  co  m 


0C00MOt0fflNNO'-lrtrt(0N1'X'*0CO)0>NC0C0tO'*iO'*OO0)Nu: 
NMMVH^HDfiOfiOiOtDOlONNKiHiCcrEffflOKOOrtNliHH 
^0'*^5HtO!CfflOO!OM»OlO«)(NMW'W'*COM©McOC<5'*•*CO<0,*,•* 


ss 


OOOVHtOOWO 
iOcor-~CNI-'*OCCOO 
COCOCMtOTfiirOCOCO 


M  ffl  lO  IO  ffl  (£ 


tOtOO©( 


lNINNO'*'fl'COroOfflJJO:'*f5*(NtO(N-HrHCC^N'fl'<OiO©00"C5iO 
!  t--  CO  CO  tO  OO  O  CO  '-O  LO  >C  -*i  -n  CO  CO  -F  CM  CS  ^h  00  f  -h  O  >0  CO'  C  CO  OS  OS  CO  >0  00  0C 
)00OHM000000M00»HM(»00HNrtHOOHH00rtHHOOHaiOO 


O  CM,  epos  ■ 


co  to  o  m  OS  <n 
7  y  oc  oo  So  So 


to  OS  o  to     •  f- 


OCOOOOOOOCOOCMiOCO 

coo^o-- 


OHOOOf OfWNNV 

_    CO  C  O  OS  00  O  00  OS  t-  CO  N  lO  N  N  «  O)  'O 
COCOCOiCtOOCCOCOCOC^CMcOiCC^CMtNiOCOiOiOiO-^iC 


oo  -<r  i-H  co 


00  O  O  CO  iO  <M 


00  C<5  CO  tO  f  Q  N  tO 
t-^CO'iO'— lOstO-Hio 
CMlOCOCO-^flOCOCO 


CO  CO  CO  03  CM  (M 


14<j  ©r^ 


o  o 
'd'd  p 

:  :wWehS«  : 


rfO  ©  o  c 


■a  9 

o  p 

£03 

si 


S  TJ  T5  rP  TS  'd  -p  St) 

cSoOOOOono 

Poooopopo 


rtti 


:  :  :£5?£  :  :  :  :  -.s^?*?  f?^  : 

-CCd.b  g.fa-P'P'P'd'P  S-J=!------^A  3-bT5 

•  :^ch^  :  :  :  :  :psaaaaMSffM  ' 


(<M 

Atj-ci  a 

03   O    O    03 

flOOfl 

•5.M  ©•?  j^  ^  "9 


CO  00  CM  O  00  • 


CO  -f  CO  -f  CO  CO 


i  O  t~-     O     OO  i 


CO  iO  CO  00 


o  o 


WW 


XfNrHI 


cooo        i-i 


,  CM  CO  i-H  CO  T 

d66d696    o    000000 
o  o  o  aT  ©"  ©"  ©*" ©\2  ©"   «T   <af  ©~  ©~  ©*  ©~  ©"   o 

£ £ £ "p/p/p/p/p, g<'p<  'S  ftpa'pftft  £ 

^^„t/iizic«cnc^asco      03      rr.  v.  (A  za  xn  vi 

,o',P'P,2,2,2,2.2:P.2  ,2  5552510  -rT 

DQMMOobob^'o  o  Sbobob 

wwwddddc^c  b  d<i<i<ti<i<5  d 


)    o 

-*■  £  £ 


o    o 

©    ©"6  6  o. 


05  ... 

-:  o    o    o  o 
©    ©    ©*  ©" 


•a-a^^^ftg1  &  &&  Of 


©    — 1    s 

©      —1      WH 

co  O  O 

060 


_©      v  ^ccco. 


,0  O  OO 
0  ddddo^  ^  ^^ 


000000 
££££££ 

CD  03  O  C3   ©  O 

©»«  ©  ©_© 

00000c 


pp  B  3  P  S 

OO  O  OOO 

fefn  Pm  fE<^fe000000( 

.Sf.Hf  .SP  .Sf.£f.Sf 2 3 2 2 !3 3 2  2  222222  2 

«pq  pa  pqmBOOOOOOO  O  OOOOOC  O 


OOO 

2  2  2 

OOO 


°    oooooo    2. 2 .2 

2  222222  2  22 
o  oooooo  o  oo 


oooooo 

222222 

OOOOOO 


I  <N 


iss^s^s^ 


iiOCON     00 


OS     O     — 1 


<N     CO  •<*<  iO  CO  t-  i 


378 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spi-req— pnpojd  p3i;rai 


188j— x^dap  ib;oj, 


•j88j— mdap  no 


o> 

f3 

B 
a 

o 
O 

I 


a 

S3 

o 
O 


ran:vBp  aAoqe  ©pn^iy 


•^98J— \QA9\ 


pa^iianad  ssau^orqj, 


•^9aj— do;  o;  qaddo: 


3  2  ®  £»  S 


U 


00  TO 

ffiOH 

WCOM 


OHX«5tDNN(DO 


cococococococococococococo 


IflCCIMlONOONt^NO 

cococococococococococo 


fflOtCO'3'tO' 


CO  CO  CD  CO  CO  CO  CO  * 


cccocnicoioootcot 

tcdcocococotcocd 

'COcOcOcocOcOCOcOCOcO 


lO  iH  M  t^  O  iH  00 
lO  CO  CD  C5  CO  00  CO 
CO  00  00  00  O  00  o 


'lOOlOOOO' 


OONfflNlOlOMOOiOOOOOOOOHOOOCNtDOOH 
<N  CO  CO  CO  lO  CO  lO         CO  lO  lO  CO  CO  CO  CO  CO  CO  CO  lO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  CO  00 


•300 
m  :  : 


9"3 

C3  o 

fl  o 


pqW 


i  :dq 


o d  o d  o  d^^  ad  o  o d  d  d  d  d  d  d  o 

^  ^  r&  *&  ^3  ^  »pH  ^  ^  ^  T3  X?  ^3  'O  ^  X^  'C  r^  T3  'O 

:::::  :Wpq  :::::::::::  : 


»o  lO  O  Ol  1— 1  CO  1 
—   ■'    Sj  00  00  t—  < 


Oi     C!iOiCNMt^NMMiOO'<tiiO 
00     OOOOt--COOOC7500a>OOOOCTlOO' 


6  6  6  © 
.2 .2.2  •* 
,2.2.2  * 
000  ^ 

tf«tf  £ 


"  CO— 1  CO^OlCN     00 

do'Soddodo 


CO  00  r-H  i-l 

6  6  6  6   . 

<!  Z  Z  <i  t  ,_;  ,_,  <m'  co  io"  co'  «> 

«e e«  66066000 


00    .  o  o  o  g)  ©  <d    a?    o    •    *    *    • 


•43  o 


000    o 

333  3 


CM  COT      1-H 


000  o_o  o  o  00    6    o  0000  o  o  0.2.2.2.2.2 

333333333  3  3333333333333 
000000000  o  0000000000000 


COTflOtONI 


OS  O  T     (M     COTiOCOt^i 


I  CO  CO  T  lO  CO  t-  CO 


BL.ATCHLEY] 


TABLES    OF    WELL   DATA. 


379 


t-  o  o 


IrHi-t  «H 


OOOOOOlolOlOOOOOCOOOOOOOCOCOOOO 
OaXOWiOMNNNC  i  -  C  J  « -  >G  O  3  o  O  O  iO  iO  10  <o  O  O  O  10  o 
^^-MNrtCMCO-^C^CNC^C^^^COCMOq^WrtrtlMrt^MCNrtCO 


N  ffl  SI  M  O  N  O  O  O  -i)  M  10  IO  O  O  M  ^  • 


OOCCWNOOOOMOOI 


^3to^3wco^2^3^:KMMMcocoMMNcoco?5w^;fc^orocc^:MM«)«lMc<^Mncl:MMpoo:McocoMeoM 


OMSHaOLONSOMiOHlONSuCfO 
NS>Of»rt-HTti"4"Hc<5NTt<M'VTJ«0'HO 

cococococncocococococococococococococo 


NOMOOOOiflOOOOl 

ooiooc-r.ccis  oo 

CO<N<NcOCOCO<MCN)CNcN!N 


I  lo  iO  CO  O  ' 


ilONTfOOO  V*00>' 


lOOM^MiOt^OlON' 


!03C0T*<^-(OtMO'*0i00i0- 


■*  O  N  O)  N  ■*  TP  I 

oo  oo  oo  oo  oo  oo  oo  i 

•«<-rH  i-H  O  rr  TP  rH 


5  S  C  C^  3  3  O  H  O  J!  O  f  N  3  (^  iC  X  -i  O  «  CI  rH  N  ?:  C  O  X  <t  S 

ooooooooooooooooooooooooooooooooooooooooooooooooooooooooo 


.^(NLOSINSISIOI        CO 

cocNTt<coco*rror/:rc-~cocM-Hcoco      io 
oo  oo  oo  oo  oo  oo  oo  go  oooooooooooooo      o 


o    'cocoTfCNXM     •    ■OHOOH-'OOisaL-opwfflooionwNOioio      (M 

CM      ;N«iOiOCO      ;      ;NCOCNcOCOCOC^^CONCOC^CNCNC^«CN«i^eN|<NTF<NC0<N       CO 


io^Noco^NMHooo'<rHooovooovs(NfflonHoi>cono()cc^co^oiociO'«ioffiS)Tiioo(No> 

COCOCOC^CNCOCOCOCOCOCOMCOCOCOCOCNMCNrocOCOC^CNlNCMeNCNW 


N00t--iOc3i'-l»(MOJ^iM'^05-*CN-^t^^-ii050( 

00!N(OtO<aDNNf-MS!3M10NN!Ot-NI 


®OSiONS>CO>oaNOONSiNm^iMOOT)<ONNSiO       CO*-iCit*-> 
N  t^  t^  S  LO  O  l1  lO  lO  ul  LO  LO  lO  S)  SI  ^  •*  O  O  TJ<  LO  Si  t~-  LO  lO         00  Ci  Ci  © 

Tf  ■■S'  TJ<  T)1  Tl<  T»1  -qi  "^1   ^1  Tt<  ■*•>}<  TJC   ^  TJ1  ^  T)i  TJ1  -q<  TJ1  TP  •*  r}(   -^1  Tf  Tf  TJ1   t»<  ITJ 


o  o  o; 


o  o  o 

£££ 

•a'tf'd' 
©  ©  © 
©  ©  « 


o  o  o  o 

ZZZ2 


o  o 


c3  ^  c3  c3 


iCCNt-cO      •      .00     ■      •      .O      •• 

irtt-Hi-IOOlO^HCOt^CS^HTCN 

•^w*^  6  6  6  6  6  6  6  6  6  6  6  6  6 
£ -T,jv-r!z;  £  &  ef  ff  a  pTpTa's  fl  fl  c  pfrT  df©  6  6  6 

„  ©  ©  ©     „-.,c3c3<3c3c3c3c3e3c3c3c3o3  c3  w  £  £  £ 
■Hc3c3c3c3c3c3c3c3  aS'3  cJ     --■ 
ooooooooooooocS^cSeS 

t>^ggbbt>«  pq  cc  pq  pa  pq  £  pq  nq  pq  cs  pq  &mmw  w 


%HUHHi 


o  o  o 


a  o  o  o  a  H  a 


o  c  o 

£££ 

©  ©  © 

©  ©  © 


o  o  o 


O  O  O  o 


JJ^J^WKWWW 


^--itNeo 

0666 

0  c/Tc/Tt/r 

►>  o  o  o 


.     .     .......,..,,'..          s-  s-  U  t-<  u  .  ©  ©  © 

nssss  -222 

I    >    <    1    >    ■    1    .    •    ■  j    ;    .    ■    ■    1    1    i    .    .    1    1    .    1    j    .    i-j    1    1    1    ;    ;    1    1    j    ;    j    ;    ;    [OOOOO  ;  0  g  fl 

ddo^o^odddo^o^dddo^o^o^do^do^ddddo2202222  .2  ^  £  £ 

3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  3  .£f .Sf .Sf .£f.S£  3  «>  ®  ® 

ooooooooooooooooooooooooooooooooooooooooopQpgwpgpq  OMMM 

OOHNMV'Offilt^«)0>OrtNM^rtNn^lOSlt*0001O'HNM^^S>N00OpwNMgiflSlN0Cg5O  rHCNCOf 
^H^Hrti-H>-Hl-HT-I^HrHi-H(MtNtNtNCN                                                                           HiHHrtrHrtlHlHr-lrtNNCNNNMNCNNCMCO 


380 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


•siaaxeq— ^otipoad  p3pni 


•}80j— tfldap  ib;ox 


•^93j— q^dsp  no 


ran^p  aAoqe  epn^piv 


"}99J— I8A8I 

Bas   A\oiaq»  aptvjyjjv 


'199J— 

paiBj^euod  ssau^oiqj, 


•J89;— do^  o^  q;daa 


sz 


g  . 

'43  O 
CO 


.-HIM  »H 


QP 


<M  CO 

S38 


Omomoc 


O  00  O  < 


C     /.    1-rHlOM 


'*ffl0>©00©'* 


iONrt©ONCCOMNOI 


*d 


O  O  o 

ftfto 
<s  <o  i> 

dd-£T:-~d.£!.£.d. 


i  N 


o  o  o 
o  o  o 


■d  O 

■Cd 

pa  : 


lO  r»i  h-     ■<* 


00     00  iO< 


666    6    66    6  6  ^  ^ 

pTcTrcT  ff  &  &  &  ^T^tT 

C3  cj  b£)     bJO     SuO  60     M  h0£  £ 

^_,w  c3     c3     rt  c3     cS  c3^2 

<d  ©"d  d  "dd  d  *d cc co 

^drdd  "d  dd  "d  d    .    . 


Si    t-i 

o  o 


-3-£j  O     o    o  o     o     o  o  o 

•CCS  3  32  3  333 

CQCQO   O   OO  O   OOP 


Ifc       03 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


381 


1 

S 
- 

"5 

•  a 

;  c 

■  - 
:  c 

■X 

•spzieq— ;onpojd  reprai 

Eh 

ft 

o 

•02 

'%dQi— q^dap  pno  j, 

•;ooj— q^dap  no 

C 

c  o 

00  lO 

§ 

CO 

•188;— etrejd 
ran^p  aAoq^  apnipjv 

s 

•188J— J8A8J 

o 

•?88J— 
p8^J^8U8d  sssujpiqj, 

(M  TJt          rH  i-H  t-I  N  r-l     . 

188J— do}  0%  q^daa: 

1,534 
830 
940 
1, 304 
1,506 
1,614 
1,750 
1,985 
2,152 

s 
- 
$ 

J 

IN 

c 

HP 

a 

i 
[C 

PC 

V 

c 

l»p 

c 
: 
T 

PC 

■i   | 

->> 

X 

-I(M 

pi  p 

-  - 

-  r 

5 

c 

•= 

' 

Sur- 
face 
ele- 
va- 
tion— 
feet. 

c 
cr 

CO 

"3 

"5 

© 

c 
c 

p 

r 
- 

c 

c 

.= 

1 

- 

0! 

) 

t 

i 
! 

o 
'o 

"3 

1         • 

c 

c 

1/ 

c 

S- 

PC 

p 

a 

•c 

p 

a 

o«  ■ 

C3  O 
3>B 

g    . 
33  o 
£  55 

to 

a 

382 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


o3  W) 


cow 


®-g; 


*'"  e3  03  03 

O    .cococo 


•spxreq— }onpojd  fenrai 


•^aoj— x^dap  pnoi, 


•^88j— mdep  no 


raniBp  eAoqc  opn^iv 


•;aa;— PA9I 


pg^Bj^angd  ssau^oiqj, 


189j— do*  o%  mfoa 


S  gi  *  its 


s* 


•  OWNMN 


NMOHMCOOO 


:§g; 


UO      'iflNNi 


r--  co  ic  <©  oo  oo  co 

HHCONNN* 


ll 


<ooio 


■  MOioi'vaioioMioNoooioQO'Oioo 

iiOtOiOMiOOt'"5>0'*eoNOOOOtO>OiO 


MNrHHfflHlOiflNIO 


i  O  <N  iO  O  O  O  iO  < 


t^-lO-^OOOCOt^lOCNIOO^it-OCt- 
05'«*<t>.05050'-HC^T»icOOOCOC3Cl 


MOCO 


nOHcoooxiomio 


^2 


ooNmujooooNoooiONomioooin 

C0-9'CO»tfiiO'«J<00i-tCO''*''*»<<O?OC0i-lCVlcOC0CO 


o  fta„ 


rdtJ 
o  o 

O  O 


o  o 
o  o 

44 .« 


'5s  B^Swpqs  BS&ia«PQ55  5B 


CO  CO      CO         CO      CO  CO 


o  o    o 
5555  55 


OO  O 
66  6 


o    o 


o  o  o 

55  £55 

id  ^ 'O 

3  3  a 


<35 

ft     ft   p<       ft 


ww      55      fc 


55     55 


2  2  2 
23  3 
oo  o 


o    o  o 

3  33 
o  oo 


o  o 


i-KN      CO         *     lOSB 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


383 


"S-2 
£co 


03  £ 

coS 


:8 

-u-w  .0 

CD  O)      ..J" 

JfSS'giif 

03  "*  "I  O  <3 

-305080-3.2 
COOOZcO 


SoSg 


CO  •<* 


m  «3  o  w  rc  o  o  o  m  o  t—  t-i  m  < 

/  '/  S  -  M  I-  ^  ~  O  w  (N  X  TC  I 


NOrtijifqiOlCOCXDlOHCOlON^OO 
COWrHMOiMMNOONlSNOOKNON 

OHHiOMOOOOOVVONOOO 


)  10  "O  "O        l^  CN  •— 1 

I  00  CO  CN         -H  !>•  m 

1  o  o  00      ©io»o 


to       tO>-f 


OMOOOOOVM 


ifliOOiONOVOiOOMffilOO 

rjnot>-ooc5'VTriio^ooc^oo>-i 


eo005tOOOiOiOCNT}<iOC5TJ<OiOCOtOCNtOCO 

tor^oo^HOtotot-^i-n-^ocNeNtor^cnr^Cir-- 
oooooo'^'t^oo'vooiooooo-^t^oo'voo^rioo 


no  >o  o  eo  00 
)  .—  to  t~-  00  cn 
)  ^  •*  to      00  o 


sss; 


C(NiOO( 


1  UO  tO  CO  O  iO  C 


m  m  m  co 


m  cm  o    •  lo •* o 00 o n 

.-Hi-HCN      •  <N  CN  t- .-it^  CN 


mooo 
ooooc5»-i 


lOOOOM^WiO 


co  00  o  00 


MOlMOCCWOONMOiCOOlW 


•d  O  O  q 
'CO  73  3 

pa  :  :ca 


;— <  CN 

'-OT3 

o  o 
o  o 


■3  o  u  ej 

pa  :pa- 


d  o  o 
"Cd-d 

«  :  : 


ddd 
O  C  O 
OOO 

S^  £  £  is  5? 

go—---  2 
«5 MWWH 


O  c3 

ftfi. 


otso 
s  papas 


O     .  O  03 
P<   •  ft  Pi 


t-4« 

,     -d-d' 

O     ■  O     •  O  o 
P,    •  &    '  o  o 


ej-d  O'O'g  c3d  oj-d  e3"££ 

-  pa   :papas  pa-  pa-  WW 


•O  o3  C3 

paces 


-d  ct 

PQ5 


■ao££ 

pas  W&h 


o      o 


P     P 


CN.-H  Ol 

6      6  6         6 
P     Pft  pw 


o      o 


I  5 


tf   «   « 


co  co        co  eo  co  co  co  co 


O  O 
t->   - 

papa 

CO    tt) 

d-d 
II 


c 

a 

fl 

PI 

PI 

PI 

PI 

PI  PI 

c 

d 

PI 

PI 

,y 

A 

.y 

CO 

CO 

CO 

CO 

CO 

CO 

CO 

coco 

CO 

CO 

CO 

CO 

u 

0 

0 

eo 

•V 

to 

t^- 

CN 

CO"3< 

m 

CN 

eo 

■* 

us 

to 

384 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


•spjxeq— lonpojd  ibt^iui 


188j— i^dgp  ib^oj, 


199j— t^dgp  no 


•^89J— Qxve\d 
ran^Bp  8AoqB  epn^piv 


•}99J— I9A9J 

■B8S   A\ojgq   gpn^iv 


•}99J— 

pg^j^gugd  ssgujpiqj, 


•^99;— do;  o;  md9<i 


J>  os  a' 
»  >  9. 


ss 


1° 

C3  O 
£2  ■* 


b* 


:fc 


■*        (DOCrt-tff  tOI'TOlN        nt-woo 

<M       l-NNOBI KCOCI-       i--*ioon 

CO        MiOMtONiOMCON        lO  *C  Tf<  lO  ■f 


CO         TMMOltDOT  (DtDHCO         I-CONC* 
I-         NNNOOCMi'TT  -    "M         NiOCOO(D 
-        I00O5CN        OOlOOO 


00         (M  C3  i-H  05  <N  ! 


00        OinOM"3 


iO     •  o  o  »o 

"*      'ONH 


I  O         OOOOMtO 


OOOiOOOOOOO'OM       OcOOi 
(OOOWfiOOONO        tOOONi 

cc  •*>  >o  co  co  ro  ic  co  ^r  co      coco-*' 


si 


5  c 


■  id    •    • 

5  ^   >»7n5  OT  S>   OT  i5"^ 
O^  S^O  «S  C3^3 


h(N-hN 


o  o  o  o 
o.  o  o  o 

%,  pS  £  £  £ 
c3£#££ 

2    *MhM 


Sgp« 


5  m  tot; 

O  03  o3j? 


OCJOfl 


S8 


i-;1 


c^iOTrcN-tf'-^co-^cocofO 


HHOto**ocoooi 

HMHHM  I-l  i-I  1-H  1-H  ( 


iO)iOOO«NO«NN 
'  H  »  O  -f  t)<  oci  O  *  00  00 
1")<  tC  f  lO  lT5  L»5  lO  O  W 


•*  o  o-ts  o    •    •  o  o 

o £ £  o £ -3 t3 .fa .fci  2-~ 


6      d 

.9"  .3" 

03        03 


CuPhQ 


O        O     "br      o 


o  o 


o  o 

bCbO 


£S«i    £    ££ 


o        o      o      o        o 

3     3    3    3     3 
o     o    o    o     o 


pq 
d 

:l 

o  £  o 

3  §3 

OfflO 


o  o  o    o    o  o 

333  3  33 
ooo  o  oo 


CO         t-  i-H  CM      i-H     <N  CO 


BLATCHLET] 


TABLES  OF  "WELL  DATA. 


385 


J. 

c 
c 

a 

- 
a 

e 

* 

a 

c 

a 

r 

C 

c 

= 

a 

T3 
Ft 
C3 
CO 

-d 

d 

09 

CD 
| 
3 

CD 
Si 

© 

DO 

5:1 

s  s 

ill 

ph<2"~ 

d  5-T-c 
°  ->       a. 

OO  c3  C 
S       O 

o 

1 

c/f 

ce 
O 

CD 

<E 

to 

8" 

c 

o 
or. 
cm 

o 

§ 

a> 

;SJS 
co 

i- 
o 

o 

1 

la 

.  -  s 

cs- 
txi 

— 
o 

o 
,d 

CO 

1 

co 

co 
c3 

o 

>> 

t-l 

ft 

coo 
c3co 

o 

o 

OS 

A 

>o 

g 

CO 

5C 

CO 
CO 

to 

a 
o 

8 

tC 

S 

CO               CO 

CO               i-l 
00              CO 

CO 

r 

•  ~. 
CO 

1- 

1 

CO  o 

CO  t~- 

to 

s 

CM 
o 
cc 

- 
tc 

iflWLOOOiOOH-i-iio        o  o  t- 
M©OONt»LOCOrtO©M 


-  ~  ~  ~  v.  or go  c.  cm 


onnnhn^cslo 

•^lCOCO'*'^'^1-*COCO 


ooo 

CO    T-l    ^ 

CO  CO  CM 


00  CM  t-  00  t^ 


— *    W    J .    '-^4   l^-  UU   l^-   iJJ 

■cNnoooN®* 


HiOiOOOLCCOOlOO  OOMO'HrtHHHNNNHCC 
OHCOC:N-*NOJNOO  CDSICO'-HI^CM^HCM— <-(<t— 1005CO 
i-HOtONNO)rHM'*lCtO        OO 


lONKOOOHHO 


-P  CO  OO  GO:  Oi  CO  CO'  ^*  LO 
OiOOOMNNLCO 
OHH( 


lOOOOi-ii 


CO  O  T  O  i-l  o 
lO  CO  CN  CO  <M  CO 

rtrt(NO)OH 


CI  O  iO  O  iO  »o  CO 


8S3< 


cooior-'^oooioooi 

CO        r-t  CM  CM  rfi  i-H  CM  <M  ,-h  i 


O  CO  lO  U5  lO 


CNCO000CCNOt~-^CNlO' 

COOlOHNCOiOOOfflOJ' 


W  O  ic  CC  O)  O  r- iCM-^TtiLOiCcOiO 


—  oo  rctL-OHCO 
CO  00  CO  -T  I  -  co  CO  00  CO 

TfllOCOTtlTf-^l-^lOCO 


t^COOlCNlO 


a  g 


o  ft 


fcjO 

o-d  o 
■d*Cd 


I  N 


i  eq 


!eh« 


o  o^ 


a  "d'd 
en  •  o  o' 
d„"  P  ° 
5~co££ 

w?S3S 


i-HCM   O 

III 


i-l  CM 


O  «  O^^sj^   o  «  « 

!M 


:^eh; 


ifHEH 


c2  :M 


■  -d 
o 

:  S"M  *  & 


55    ^ 

Oh       t» 


^   !3     K 


o    o 
&o    CO 


+3     T3 

C3     c3 


« 

pq 

d 

pi 

CO 

T3 

TS 

^ 

* 

J2 

^; 

pj 

a 

CO 

3 

^H 

~ 

fl 

.d 

^J 

•d 

a 

3 

0 

CO 

CO 

CO 

o 

O 

o 

0 

O 

c 

O 

c 

o 

LO 

CO 

CM 

CO 

lO 

CO 

CN 

-25  G 


386 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


•3 
0) 

fl 
'■£ 

d 
o 
O 

I 

•si 

CO 

© 


•sxaJJBq— ^onpojd  leprai 


188j— q;dap  pnoj, 


•»aei— q^dop  no 


•^oa; — QWB\d 
rarnBp  OAoqe  opnipiv 


•^8aj     \9A9\ 

B8S   Aiopq   apn^t^y 


CO^O      'O 


ss 


io  o 

ICO 


:8  :J 


ONO  lOfOlf  OlINOWOOOlOOCt'DNLOlOlOONONHTfiOll 
HWH  (NMtDrtOOMO:t~COOlO'«l1'lOlOHkOHN<OCO«5N'*N( 
>C  CO  CO       CO  C<1  CM  ic  "31  CO  CO  *C  iC  >C  CO  CO  «C  IC  CO  »c  co  »c  >c  -^  *C  CO  iC  iC  CO  IC  ' 


CNTCi  OHHO)01fll01H01»H0100  010100100  0>( 


N»H        HCtOOiONHuOtOONNO)      •      'WOO      'OlNrtNOiOO 
CN         i-H         r-<<M(M,-<         tH  i-I  r-H  CM  ->J1  (M  ,-H  .-H  rH       •       ■  i-<  CM  i-H       •         rH  CM  CO  iH  CO 


•;99j— doj  o;  nidaa 


ft  • 

C3  O 
3£ 


iCCOCOt^COOlCO 

'  tr  o  t^  eg  55  >c  >c 


iC  CO  CO  CO  CO  CM  CO  < 


w^a 


:  >> 
.id 

« 5  ■ 

P3  T^TJ 


t3  t3    •  "C 
o  o    •  o 

o  o    •  o 


■a  %o  °  %*  °  «s^  °5£  ££*  s -a  *ts  © 


I 


CO     CO        CO 


CO     CM 

6    6 

£  £  £  £ 


<2   B 
o 


©©ocuoooo 

S      3      gj      3    £    fc    ££ 

C3c3c3_cj        -       .,       __ 
■O    Tl     fl    fl     ,£5    fl    ^  (>, 


a  aaaasss^ 


•<   <<  ^  a  a 


«  pa  pq 


a  a  a  «  oj  «• 


.a   a 


.  o  o  o  o  o 

^  <»  <»  <o  oT  aT 

•S  C3  c3  C3  C3  C3 

.tj  CX  W)  W>  fcuO  6JD 

5  ftftft  ph  a 

"^ftftft  ft  ft 


,3    .3 
O    O 


oooooooo 

3  3  2  3  3  3  a  a 

o  o  o  o  o  o  oo 

<N     CO     rt<     «C     CO     C--     00  C75 


3    3333 3  3 

O     O  O  O  OOP 


•rt  o 
2£ 


BLATCHLET] 


TABLES    OF   WELL  DATA. 


387 


!  03.5 

;Oft 


«  e 

03   s- 

^   O 


^5 


co£ 


ft 


cn  jo  co  io  co  <m 


rj<  00  t-  CO  CM  lO         CO  CO  ■>*<  IN  tft  CO  CO 
to  O  iO  15  ®  ifl       lO  -^~0  CO  >0  Tf  CO 


00rt00CO(DNC»' 


i  n  io  n  o>  h  o  cr.  ci  c  s  /  x 


lO  lO  lO  00  N  CO  O)  C7)  CO  to 

^flCD00i-KMO5O5t^(MCO 

-<fCOiOiOiO-tfi"CH''*icoC<l 


iHtOtOOOlOMHOtHOOOOCilN 
CO  iO  M  O  N  ■*  CO  ■*  CO  O  N  CC  [^  /  CO 
O^QOOOOHHOOO)HHtO>OH 


O  W  00  LO  CO  05         ONtONHl 


O  i— I  OO  C75  < 


i  OS  CO  CO  O  CM        CM  < 
r-KNCNi-l  IN        CNi 


iO  O  CO  O  O  w 

Ol  W  CO  N  f-i  00        OCOOi'HOONi 

03  CO  CO  CO  CO  CO   1<  ■*  00  CO  CO  Tf  I 


_  )  CO  i— I  CO  O  i— I  CT> 

cNcoco'ntooi^oooicoLn>ninNcoincooo-<i'inm 


i  iO  Wc"  -"C*  ■*  ' 


5   W 


§8 


,  .  >» 

^  ftO     "^ 
52  oo  b»  >i  2 


S      -.2.2  co  ©  MJ^w  «J2.2  M  £  C0J2  W>£  00,3 
«o3Qcc3©'^0303©OO=«*aO,2*SO 

*j  laasSwSs  Has?  M^amMSa 


KN^ 


O  cc5* 


o  o 

32 


W>co 
T3  o3 

'SO 


££o 

•S.S  o 


.a  go-- 


I -d-d 
o  o 
o  o 


■g-a 

mm 


.fend  go 


CO      CO         CO         CO 


£  5? 


M  M  ia) 

,©  ©  ,© 

ft  ft  ft 

ft  ft  ft 

<1  <i  < 


<    <    <      < 


H      N     MO 


o 

o 

o 

o 

o  o 

o 

o 

,_J> 

,_r 

,_r 

] 

i— TV-?* 

_J" 

? 

03 

c3 

(Si 

IS1 

03  03 

03 

cd 

£ 

£ 

* 

£ 

££ 

£ 

£ 

CO 

CO 

CO    CO 

£ 

£ 

£  £  ££ 

* 

£ 

W 

H 

H 

H 

HB 

H 

W 

i-l  CO 

6  6 

03  03 

t*  £ 

CO  CO 


C 

^  ©  O      6 

•H  t/T  C/T      CO 

.  'o'o  "o 

-^  pqpq  pq 


*->  l-s     l-T> 


J5  ^  ^ 
o  o  o 


2     e 


c3      c3     03  c3        03 

sees    s 

CO    CO     COCO        CO 


£>  O  O  <D  O  G> 

se  iti  ti  tocB  to 

c3  c3  c3  c3  c3  o3 

CO  CO  CO  COCO  CO 


©  CO  00 

5    5    5 

111 

CO        CO        CO 

■8     «8     »a 

o 


CN 


W 


IOCO 


fl  CO 

^  03 

ft  CO 

CN  CO 


sa 


sc    oo  _o 
co   OO   O 


■f       if}    tot» 


388 


OIL  FIELDS  OF  CRAWFOED  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spueq— lonpcud  fBt^ni 


■199j— q^dap  pnoj, 


•looj— q^dsp  no 


^3 

a-' 

.2 

o 

O 

! 


t 

-t-a 

s 
3 

o 

s 

e 
■3 


■%99}— OUB^d 

mtHBp  8AoqB  apnmiv 


•^98J— I8A0J 

B9S   A\opq   eptupxv 


199J— 

pa^iprrad  ssau^orqj, 


'198J— do;  o;  q^dea 


t».2  ®  >.2.S 


Ah   ©Ah, 
C35-1   S3' 


C3^ 


ah** 

ioo^SoS 


O  O00(NOOOO  OLONOOCO  <M00<N 
00  HffiaJHiOO'*  IOINCOCOO  COOJH 
C3        t^  CO  »0  O  -*1  ■"»<  CO       O  i-O  ■*  CO  -f        co  co  co 


O  ON)  CO  O  O  O  O  lOOWNN  00  <N  < 
OJOMOllOOtD  Tfi  t^  CO  CO  CS>  COOI 
NOOOCOOHH  ffflOHO  HHi 


CO  00  CO  >o 


i  oo  r-~  w      »oio 


00        Oi        CN  <N  CO  ' 


&  : 

&  : 

bo 

-d  o 


255 


fcD  ™    ^  3   ®         ,2    ®  5 

t3$£q2.    o2o 
■sc5--«2    "2o 


Q    ft 


oioioo 

■«*i  t-  OS  t— 

t>-  co  n<  to 


NNONiOIN 


t^  i.O  OS  O  O  ■ 


S  'M 


31      r^  co  c 


o  o 


as 

coco 


C3  O 
S2 


§     . 

•rt  o 


o  o  «  ^  «   ^ 
££  dodo 


mwJ  a 


w 


h'HODO  O 


■8 

ooa  W 


-<  2  2  2  2  .2 
o2223 2 
aoooo  o 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


389 


(NO 


C3  O 
0£ 


CO  CO  CO  CO 


oorooio 


0)'*C<!MlO>OHOOi-lrtT)<OC»r'lOC<INtOlONlONOlOL'2Mi 
<J(OlOtONOO«)COK     ' 


iLOO^fOeoOlOTticSIOCO'tOMKCOOlNO 


r-l!DNNlOlOO>N05C3<DOHCOlOOO«1'lOCOlOCOH( 
OHlOHT 


nOOtOWN' 


lO  CO  00  O  O  ' 


O  (M00CO        7-H 


'  (ft  N  O  CC  C  "O  c<!  C  C 


COi-ICOCO^HC3>-l<NCOCCCOrHCN) 


O  O  O  lO  O 


OOOi-0>0(NTl<lONOMiO(DNiOr-lOLO'*OOaiN'OINHOlOHaiHO)00(NiOOn<00«:OlOU5'V!DM 
mCOtOO!OHOOHtDOOlONNOHHM<OOOCHONHNraO*OMOOCCCOKt>OOOHOOOCN 
COTl'TfM<OCOCOM*^0«^COCOffl©ncOCCCOCONCOCOTli*lC^COC<lM'*lOiOffiCOOO«COOOHMCO'*>0 


.       'i-KN       . 

..»  .  .  0  .  .  .  :m%mx  '.m  §^  § 


25 

.     fto 

1  "fl^ 


•  o  °  03 

^-  o  fta, 


c3  c3-g_t-.S 


CO 


c 
c 

•RC  so-- 
Mean-  W 


—l  (N 

o  o 


CO  CO  CO     CO 


o    o    „ 


o<1 


o    -  o    o 

C3   C3  C3      c3 

C3     .   c3      C3 


Wtftf   tf       P3 


o  o 
•    •  bo    W) 


£  55 


£    fc    j»  j  ^r 


o 

o 

fc 

a 

a> 

© 

ft 

ft 

Pi 

Ph 

O     O  CO     o 


2  2  2  .2 

ooo  o 


o    c  o  o    o 

2  352  2 

o  ooo  o 


AAA 

ooo 


pq 

pp 

a 

a 

•c 

■d 

* 

£ 

o 

o 

a 

a 

1* 


390 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


spxreq— ^onpoad  imirai 


•;88j— tfldap  t^oj, 


•%Qdl— mdep  no 


c 
O 

! 


uin:vep  8AoqB  apti^y 


198J— I9A8I 

■eas    A\opq   epnmiv 


•189J— 
pai'BJ^OUOd  SSailjpUIJ, 


•^89j— do;  en  iiadaa 


ic3 


c/T  P 

<3  O 


i—i  t^  r— 

-v  O  N 

■*  O  O 


^2  : 


8  :; 


ONlQO 


§2 


£■2- 

ft 


COiOiOOiOCOOJMTtiMOiOLOiO^iOiOiO^COLOiOTfCO 


O  O  00  LO  !D  I 


^OfNOOiOOt^i 


H^COMHWCOCSrtHINH  <M  .-Hl-H  1-H        .T-I.-KN 


--  X  '.r  -CHCI-C  CO  i-  CO  I 

co  co  co  co  •<*<  cj  o  to  ■ 


o  „ 


o  o  r?o  o  o 
o  c^  o  o  o 


^P 


co    co    -f 


)  CO  CO         CO         CO         CO 


fc  z 


t-l  lO  W  CO  ^H 

6  d  6  d  d  "^  *"! 

££  £  £  £  ©  o 

.  -.  .  ~  -  £  & 

d  a  r)  a  fl  _r  _-> 


o  o    o    o    o 

AA    fl    il    ^3 
H&H     H     C-     fH 


£   £ 


o    o  o  o 


£   fc 


DO    O    O    O 


£    * 


m     w  PI  CI 


Ph      Pm      Pui 


S£ 


"2  o 
en 


o 
S.S2 


AAA    &0    a    A    A    A    A 
O    O    O    PhS   O    O    O    O    O 


.2  .2.2.2    .2 

A    AAA      A 
O    OOO      O 


N     00     O)     HN     M 


BLATCHLEY] 


TABLES    OF   WELL   DATA. 


391 


>  cotS 


o  05 
c3  9 


C3(M 


■/.  — 

03  CO 

o 


O  r-  t-  t- 

•^  CO  CO  CO 


1^  1-1 

COlC 


CO  00  O  O  IO 
lO  CM  CO  (M  CO 


CC  N  ff.  O  C)  H  CO  f  M  io  O 
iOCOCO'"tf|iOCDCOce-*t<CD-tf' 


t  -C  -h  r  r-  cc  t-  c  ^  :c  -  -  -  -  i-  :c  K  s  io  c 
eo  es  to  en  io  t  ■  ~  co  ~  >  ~  i  *  co  './"  i  ~  c<i  i  o  -*  ci  -*<  oo 


lOHtDH 

_    .  J  if  M  S!  iO 

M  O  ^  CO  CD  lO  O 


CMcMOCO-fCOCOiO 


<N  «5  C  l^  I 


'OltOKfflt" 


cd  -p  as  cm  as  i 


I  I~  t—  CO  i-H  OS  ' 


i  CO  l^  CM  -f  iO  O        O  O  iO  t^  O  OS  ' 


as  cm  co  as 
f  as  cm  oo 


MNXCOCCNX'HCCN 
H  (C  IO  <N  CO  H  1)1  CM  I-H 


IIOCOCOMCNCOCOCOCCCNOcCCNl^iCCMCCNCO        LO  ffl  M  IO  lO  CO  CO  « 


OS  CO  CO  CO        CO  iC  CO  CO  f  C  O  CC  CD  ' 


CO      CO      CO         -* 


CO  CO      CO 


■      CO 

■  O  CM  -P 

r-i 

o 

CD 

.      .as 

o    o 

H 

o  o  o 

o 

6 

O 

:     ;  o 

fc  fc 

£££ 

£ 

OS 

IO 

00 

fc 

fc 

CO     ^£ 

S-'    fc.'    U 

^ 

o 

o 

o 

^ 

jj 

O    o  c 

Eh    Eh 

£<&& 

H 

£ 

SZ5 

fc 

Eh 

H 

£    ZFH 

OJ 

a> 

05      05  05 

03      c3 

C3  03  p 

art 

b« 

cct 

c3 

a 

03      C3   c3 

C( 

M 

hO     fcJO  60 

X 

F 

F 

OJ 

OJ 

a> 

ft     ft 

ftftft 

— 

ft 

ft 

ft 

ft 

ft 

ft     ftft 

ft     ft 

a 

E 

c 

ft  ft  ft 

ft 

ft 

ft 

ft 

ft 

ft 

ft     ftft 

<<     <J 

M 

«<««!^ 

<1 

<) 

«*1 

< 

<■; 

<3 

<     << 

tf  « 

F 

««P5 

« 

« 

ti 

pi 

pi 

pi 

pi  pipi 

^  <j 

d 

C 

c 

<^<|<j 

<; 

<j 

< 

<i 

<< 

<< 

^   <-<j 

O     O     o 

£  £  £ 


o    o  o 
525   ££ 


©  O_05 
ft  ftft 
ftftft 
05      05   05 

ft     ftft 


03         03 


:  :  J 
:  :  ■« 

o  o  .£P 


a 

rt 

o 

b 

o 

js^:^ 

rf 

J= 

fl 

3 

,3 

fl 

£1 

,CE! 

rt 

A 

X 

fl 

■=■ 

,Cj 

^^ 

P3 

03 

c 

o 

s 

s 

s 

oco 

c 

o 

c 

o 

o 

o 

c 

CO 

c 

O 

o 

c 

o 

c 

OO 

o 

o 

CM 

CO 

*tf 

iO 

cor-  oc 

- 

CO 

•"H 

CM 

CM 

CO 

rr  io 

se 

CI 

co 

-T 

iO 

CDt^ 

X 

OS 

392 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq — lonpojd  p3T;mi 


•*89j— tfldep  iBjo  j, 


•199j— mdap  no 


•^aaj — zwe\d 
mn^p  QAoq*  epn^jv 


O  CO 


NiOON 
rfi  Ci  Tfi  CO 


NOOC*T)<CON 
CO  CO  CM  "O  "O  O  iO 


"188J — J8A8J 

B9S    Avopq    apnixixv 


•189J— 

paiBJiauad  ssansprqj, 


•188j— doq.  o;  mdaa: 


3  %i3  «8  S  « 
w£  <d  >.2<£ 


S 

c3 


02 


NW         i-4  00  O  CD  00  CD  ' 
CO  t-H         t--  C3  CM  "O  lO  CD  i 


lOiO         O  GO  CD  CM  O  'O 


rt  CM 

o  o 

o  o 

MM 

MM 


>>>>>> 


So 

a  o 

CD    fe. 


>,>  <si  v)  z~ 
o  o  o  j& 

o  cj  cj.-tJ'C.S. 


coo 

CD  CM 
CO  l-O 


t»Ti<NCiiTi4*fLir«inNi 

05000t^CM^i-*CMCDCMCO' 

-tficococMiocoinco-V'tficM' 


i  CM  r»4  CO  lO  • 


Ci-lrtN© 


occomwinwiooHNOMNeo 

-       ■fflHOONOINOONOHOlO 


CM.-lrH  CM 


!  CO  lO  lO  CO  ^ 


-r  -r  -r     -f     N  CN 


•  !  —i  cm  •;;!•!;•;■;;.;:  • 

g    .XM%M    -M%    -M^M%      ^o    •    ■§ 
•H  £  o  o-"  or5  o-S  H  o-~  o-K'd  u.s  £o« 

Message SM^gMSM  :SMfrs  M 


o  o 

Tfl^HCM     co     'Z^ 

odd    d   .9.2 

-  -  -  ~  c3  c3 
>>(>>>,  >>  ^^ 
c3  cj  c3     c3    ^  " 


a  a 


q  o  m 


Si  S- 

o    o 
W    M 


ooo  o  as 


o    o 


,d   fl   ,3    ..q  .  .3 

O   O   O     O     O 


BLATCHLEY] 


TABLES    OF   WELL    DATA. 


-- 
1- 

v 

r 

0 

c 

c 

B 

- 

IS 

oc.,_r 

„o 

t-,00 
©00 

"c3rH"> 

s 

03 

CO 

Salt  water,  945  feet 

Hole  full  of  water,  1,115 
feet 

£ 

09 

DO 

•  a 

'  c3 
is"© 

3* 

IN 

coo 

S3 

© 
03 

"eg 

ilj 

WS?«2 

OCN1CO 
*"*  03  O 

"o3«°- 

^J  © 

03       "? 

to 

to 

IC 

c 

O        1ON1-C  >S  O 

P.*f 

p 

3 

S-i 

P 

>> 
P 

8 

s 

P 

CM  WN 

t-r^oo 

TFt^CO 

IS  t~  00 

IS 
IS 

o 

O 

co 

o 
r^ 

CO 
CO 

CO 
O 

-£ 

1,485 
1,397 
1,427 
1,367 
1,400 

o 

00         CONK50MLOO 
t-         "*t<  IS  O  t^  O  TT  CO 
CO        ■*  ■>»•  •<J1  CO  •«*<  IC  t— 

!C 

— 

NfllHOCOi 


X    --CCNMHOKM 


oo  eo  eo  oo  oc 

X   CO  t>  CO  i  S 

CO  IS  tji  -^  CM 


NNOMCOON 

o  i--  oc-  oo  co  >o  ^  — i 

OOOOt^cO^fCOCM 


CONH         lo  -^ 


eo  »-i  o  o  •«<  o  t    - 

o  c  ti(  o  «  c  r.  '-  i * 

00000)00 


t^  t-  IS  IS 

O  O  00  o 


CC  0>  .-I  CM  <M  CM  —  CM  IS  >S 

COCNOOINOON 


CM  t~r^CM  CM 


0C0CONCWO0C 
OCMCM.-ITt--rf.COOO 


i  CO  O  i-H 


rH  CO  CM  1-H  lO  CO 


!§§: 


OC  CM  O        O        O  IS  lO  O  O 
ONO         O         IOt»(OO0C 

VOO        O        N  cc  ■»  O  CO 


CO  CO  lO  CXI  IS  Q  IS  i 


-    -   -  IS  CO  'O  CO         NOINM         CO  CM 

o  c:  o  ^  cm  co  co      nccNo      colo 

lOOHMCCt-        OONN         tjc  t}< 


o 

c3 

o 


T3      ■      •      -T? 

o    •   •   ■  o 
o    •    ■    •  o 


c3^  c3  c3-^  3    -, 
0«iO:-0  2 


©  tr.  <* 


5  £   •  £  >,  ^  .2 

I  ©.£3*0  ©J- -SJ  O 


Pi  CT3 

c:  c3  c 


^  t^K   ^2  M)    .      .      .^  S  ?  © 

p=co^  WS       m  :  :  :mp:W^ 


^1 

©.3  £  © 


rH<N 

o  o 
o  o 

^^ 

WW 


-•/MCSO' 


a  * 

ii      to 
Q      M 

© 


o  o 


6  c'2'  6 


©  © 


©  ©  P  © 

a»a«g 


^^i>i^^: 


^     K 


^•C^    S 


©  s 


o 

o  =y 
coooooo^,$f 

3 S  S 3333*  g 

cccocccK o 


-H     — <  CM 


w 

i^ 


Z    CO 


IZ 


394 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spjj'Bq— jonpoad  teprai 


•198J— q^dgp  \v%o  j, 


r-<CN  TP  OOO 


•}99j— Hldap  no 


•;99j— aire^d 
ran^p  9AoqB  gpnmiy 


»o  >o  in  ©  >c  io  to 


Oli«HHHMif5l»l(3N-.. 
«5M«OCWO(S1<*TfiW» 


199J — J9A9J 

B9S   Avojgq   apn^jv 


NwiOMOOtNONiO 


:-  I  -  ■-  -r  oi  O  ■ 


•}99J— 


(oaooiwoooMnoc 


—    S  ■-   S   r>\ 


199;— do;  o/}  md9c[ 


i  Oi  ©  Oi  N  -t  -t  IC  ^  ' 


o 

•is 


^T3 

o  o 
o  o 
fe  fer 


6-OSf.M.MS 

T3  Tr)  ^  •- -3  O 


o    •  o 

f-  a.  f- 
■S  I'M 

3  S3 


ft    •       O-^  Oft    .^ft 

'CO     -~  o  •£  '£  xJ  o  'E  o  J3  ^ 


5    O    ©    03    fl  % 

m£  ©  >.2& 


CO  tH 


:s    z 


^H  (N      CO 

6  6 


©   ^  ©  2> 


.a  pq  ^m 


£^    £ 


o  o 

££ 

(/)     ro  <<  <4    O    O        O 

©  ©     -    -  C  O     O 

i^^COCoSS     S 


coo 
££    125 

i-H    aTaT   oT 


^    ©  ©   ,© 
^_T   ft  ft   ft 

r<      ft  ft     ft 

to  <1-<    <{ 


^>  > 


6 

C3 
03  O 

2* 


©z 

CO 


+j     o     o  o  o 


O   O   OOO 

CN)      tH      CM  CO  TP 


:  a  rt   a 
■  tcyrj   «3 

•  ©  ©      CD 


o      o  ooo-b-t   i 

3    3  2  2  2  g  ©  § 

O     OOOOOO   o 


Ifl 


fc      CO 


CO  l-»  00  CS  H  CN     CO 


sss  a 

CO    COCO  CO 

©      4)  CD  CD 

sa  cc5-  5a 

CO     COCO  CO 

l-H       CM  CO  T»1 


BLATCHLEY] 


TABLES    OF   WELL   DATA. 


39< 


as 
'i. 


C9 

©£ 

cfl 

08  « 

£ 

►  h 

+^ 

og 

•a* 

PS 


ft 


CO  O 


CMNCON 
h  or.  (N  K  (O 
CD  "*  CT>  OS  CO 


O  IOO  o 


o    -co 
<N     -ooco 


COMtOOOMfflOH. 

Oioooaifl' 


>  oo  o  cm  ^  or  co  or  cc 


if?  — i  — 

t^  C5  CM 

CJ5  CO  CO  ' 


1  tt3  l-^  i-*  tfj  LT 

*0)coffl0m 


:  if?  ifl  ^h       (M  ^ 

■  i  ~.  co  ro       co  co 
:  ro  co  co      co  co 


i  CT>  <N  Tf<  CM  CM 


lO^^XClOHH' 


fWLOC!         00  CO  <— >  Tfi         IOOOO 
CM  T  CO  CD        CO  CC  >0  LO         ClOCO 

f»HHH  HOCOH  ©HH 


HIONOIOU3MO  lO 
r^  — w  _^  r^fi  r^_  crt  i — i    r   at 


O  CO  O  00  ' 


■  00  CO  CO  00  CN  CO  rffi  LO  i.O  -t<  00  00  (M  00 


>  lO  CO        lO  CO  rf  lO 


t0t>,t0 
T3  C3T3  O 


>>o  >> 


o  o 
o  o 


-soft   ■ 


^      •  *•»>■    •  —  cu  o     ■     •  ©  ~    S>  ©  ~    fe->>j>-tte-a)     •;: 

r/l   h».  CO    S~     'J!:    tO-if    S^     ■    SjC  '  rr,    &    tO  rr*    P*    ^   ©  ^   ^    tO     •    rr 


°  °  S 

to  to  2 


T3  O  e3 


O   O  o 

oao 

*&* 


:1i? 


o#    • 

K/  ICC?     < 


:§  :1s 

:  *  fro 


Is 

£o  o 


o    o 


ft  a 

ft       ft 

<!   ^ 


ft  ft 
ft  ft 
<      < 


OS        or 

CO        CM 

d      c 

c 

c 

CN 

c 

•>* 

c 

CO 

6 

6  6  6  6  6 


a)  d)  o  d 

tO  tO  tO  tO 


c  o  6    fcc  to  to     to  to   to 

Z^Z    C  C  C      fl  C    C 

!.:  s-r  c  5  5  5   2  5  5 

O*    O  M  —11—1  HHI— I 

botobo     >,  >,  >>        >>  >,     •>, 

.S.S.S  g  h  ha  e  e 

03  CD      © 


K 

o 

d 

o  o  o  o 

o 

o 

o  o  o 

O 

O 

OOOO 

O 

O 

ooo 

A   si 

^ 

d 

rf 

to 

to 

to  to  to  to 

to 

to 

to  to  to 

c3     C3 

C3 

1 

fl 

c  a  c  c 

C 

C 

c  c  c 

a  a 

02    02 

a 

a 

a 

a 

PI 

c  c  c  c 

C 

c 

C  fl  c 

cC 

cC 

CCCCCCCC 

cC 

CD 

© 

©  ©  ©  © 

© 

© 

©  ©  © 

=3    «8 

■a 

«« 

■8 

tf 

tf 

pi  Pi  pi  Pi 

Pi 

Pi- 

Pi Pi  Pi 

(4 

=2 

cS 

c2 

c3 

c3 

c3 

cs 

«=    fc 

^  is  is 

.- 

c 

03      C3 

^3   ,a 

C3 

03 

C3 

d 

c 

c  c  c  a 

a 

c 

c  c  c 

sz 

s 

3 

~ 

^3    ^ 

02     CC 

CO 

CO 

CO 

o 

o 

DOOO 

o 

o 

ooo 

C 

c 

o 

C 

o  o 

O     t>- 

00 

Ol 

o 

^ 

CM 

CO  -^  lO  CO  • 

r^ 

oo 

ISOH 

^H  CM  CM 

o 

CO 

lO      CD 

396 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


spjjiBq— lonpojd  i^rai 


laaj— q;dap  pnoj, 


•;89j— q^dop  no 


ran^p  GAoq'B  9pn;p-[v 


•^88J— I8A8I 
■B9S    Ai0[8q     spnjT^iY 


pa^ej^augd  ssan^oTqx 


'199j— doq.  o;  md9(i 


O   ©    C3   fl-g 


o 

a 

o 
d 

C3 
c3 

'   P      • 

■  •2   •' 

ilj 

:dS 

•  t>    .N 

;  cx>> 

Jit 

•  g^ 

a 

i~ 
y 

rr 
c- 

o 
,o 

IO 

09 

o 

o 
03 

o 

So 

<£<2 

i-H   CO 

c3  a 
OO 

O 

OS 

o 

iO  o 

co  o 

TJI 

of 

oo 
to  IO 

O  O 

IO 

1  - 

CO 

o  co  cm  co 

so 

CO 
OS 

iO 
SO 

asio 

lO  i-H 

COCO 

CO  CO 

30 

CO 

O 
CI 

co 

as 

OS 

OCO 
CM  CO 

CO  CO 

r- 

lO 
CO 

CO 

as 

CO 

CN  O  lO  io 
OS  OS  CO  I-- 
IO  CM  CO  IO 

osc< 

70  7C 

0 

-f 
oc 

c 
c 

s 

2 

co 

OS 

CO 

l^  iO  CO  CN 

©LOHH 

>o  CO  iO  CO 

too       OO  CO  ■ 


Vl^OOrtCCWO 


O  CO  CO  CO  CO  CO 


'C0O>0C0TPC0i0Tft0t>.O 


HOtouOH        CM  ^  CO  CM  < 


TtHNNHH'* 


CO  iO  O  O  OS  iO        t—  OS  CM  CO  CM  iO  CM  O  O  O  'O  O  iO  00  O  iO  o  o  r~  iO  CO  CM  CO  CO 
CO  "O  IO  CM  CO  LO        CO  CO  CO  CM  CO  CM  < 


o  >>>> 

Sou 

^   OOi 


£.2 

£o 


•d-P' 

o  o 
o  c 


o 
o 

=  *=*' 


o  o  o 
o  o  o 


*  :£I1i 


Kg 

o 


f  f  P-w  P-"co  t>>  ^  «  °  5?0  &£  £  JS  £  &>£ 

;.;_'  o    .s.a.sc.sc  ^-.p.s.s  2  o  S  o  C.S.H  »g  o.a  S 

t4a    54^-  ^^^ehSe-^p^^S^pi 


CO      CO      CO 


CO         CO  CO  CO     CO 


CM     CO        CM     CM 


o    o 

55  £ 


o    o 
55   55 


o    o    o 
55   55   55 


W  M  M 

H  r1  H 

o  5  S 

Ph  P-<  P* 


6      6 
55     55 


55      55 


a 

C3 

c3 

00 

e3 

O 

o 

Pi 

Pi 

P 

a 

P 

Pi 

Pi 

P 

P 

P 

<< 

< 

< 

< 

< 

o  o  o    o 

555555  55 


WWW  M 

■~  -  •-.    - 


<t1      <J      <sj 


S55 


02 


o 

o 

o 

o 

o 

c 

O 

o 

o 

o 

o 

o 

o 

o  o  o 

o 

|c| 

^ 

rP 

X, 

p 

-P 

A 

Pi 

A 

p 

p 

Pi 

Pi 

Pi  Pi  PI 

p 

O 

O 

c 

O 

O 

C 

o 

O 

O 

O 

C 

O 

O 

OOO 

C 

!>• 

oc 

OS 

— 

CN 

CO 

iO 

CO 

t^ 

CO 

OS 

rtCMCO 

1^ 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


397 


s  a 

00  o 


C3J> 


<M  — H  t—  C5 


uOCM 

7-    - 
OitM 


OMNM 


y.  io  si  ■-  >o  i  - 


OOHNfflOOOCmOOlTJNOt^i-OXa'ffi^ 
O^OTfiOO-^iCMlM-^COCO-zrt^-^aOIMlO 
N(ONtO(OtOHO< 


oiooffltoo 


H<0<JiNO)0.«5«5 
i-H00i-H-0n-ICCa>eO 
JO  iO  «>  CO  ffl  05  SO  (3 


UO  CN  O  CO  M  w  m  CN  CO  LO  CM  C-  X  ^  v  —  co  c-  c  -/-  X  I 
WC0^"rHO^05l0NCNlO1,00n<NCN00lOOO1,i 
OtDtOtDOOtOtOOOtOOOtOMMtOtDONtOI 


NOlCO'VlNcNMNiOCO'^MiOCN 
ffiiOOOHLONNiOCOtOiOMlO 
t^  00  I>  00  00  CO  CO  Tf  00     " 


-*  CT>  00  00  00  1* 


INOtOtDlO       'OOOiOO 
Ir-ICO-fCOia      •  N  H  M  N 


i  CO  CM  CO  lO  00  CO  CO  t 


CO  CO  rS-  "O  —i 


^wO>antOMtOOOOlOmtOMMflOMt»t»t>Nll5lO 
CM  O  Ci  CI  :-  -M  -  /   O  O  r-  X  'f  O  LI  rt  LO  X  CN  CM  OP  CN  O)  O 

oc)cocMcooc3<MCMcx)oe^c»CT<Mioco(NC<i02CNeqc>iM 


aiioo-^r-; 

CN  CM  CM  CM  CM  CMC 


CM  Si  O  O  CM  30  £-~  O  lO 

sc  co  o  r;  co  x  f  h  ca 

M  7>  CO  X  CO  CM  CM  CO  00 


O  CM  iO  oo  a-  CM  CM 


fc-tf 


is! 

!?5 


005 

ft  ft  O 

03   CD   |> 
MM? 


0  °o 

O  ftO 


o  ft 

(>  03 

^T3 


Mo 


000 
000 

—  _—  _  ^*     _ 


— 

3 

o 

•no- 


O  o  o  o  o 

ft  o  0  0  ft 


-o  «- 
0  2 

~     fe  03 

~  ?  hi) 


So 

o  ft 


ftMMMft    !::  Mft    '.Ma    *.  M  «2  !i ::  M 


ft^ 

-J    C3£    tfrg    O 

pq^  Ms  m  : 


CO      CO     CO      CO  CO  1 


00         CO     t~-      TT 

CO         CO      CM      CO 


CO     CO      CO 


fc    5?    fc 


O      O      O      OOOO 

£  fc £ ££££ 


bfl 

bii 

bfl 

buri 

bj 

Wi 

a 

n 

Pi 

d 

d 

PI 

a  pi  pi  a 

M 

M 

M 

M 

M 

M  MM  M  M 

>, 

>, 

>> 

> 

> 

>, 

>>>>>>>> 

e 

E 

L 

0 

03 

03 

0 

OJ 

0 

03  03  03  03 

ft 

ft 

ft 

ft 

ft 

ft 

ftftftft 

hh  a  £  £ 


OCOOOO         OOO 

££  £  ££  £    £  £  55 


OOO 

fc  £  £ 


03       03    03       03 


I* 


WW  W  WW  W    W  W  W      W      WWW    Wo 


0 

0 

O 

0 

O 

c 

OOOO 

0  0 

C 

O 

c 

0 

0  b 

C 

O  O' 

c 

O 

0 

0 

0 

0 

0 

O 

O 

Tl 

~ 

A 

J 

rd 

A 

A 

AAAA 

AA 

A 

.= 

.a 

A 

J3^ 

A 

^^=! 

A 

A 

A 

rt 

13 

A 

Jd 

-= 

^3 

'~ 

3 

C 

c 

0 

0 

O 

OCOO 

OO 

C 

c 

0 

O 

OO 

C 

OO 

C 

Z 

Z 

O 

0 

0 

0 

c 

O 

ft 

CM 

CO 

T 

CO 

NKOO 

rH  CM 

re 

m 

CO 

i-H  CM 

CO 

TH  IO 

CO 

r- 

s. 

- 

0 

rt 

05 

co 

rt 

398 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


spjjeq— ^onpojd  i^rai 


188j— q^dgp  \eiojj 


•^99j— q;d9p  no 


55. 
CO 

O 

Eh 


•399;— QWB\d 
ran^p  9Aoqe  epn^i^y 


199J—  I9A9J 

■B9S   Aiojgq   gpn^T^V 


-199J— 

p9^Bj^9U9d  ssgnjfOTqj, 


199J— do^  oi  qid9(i 


t3  ® 

w  O 
C3CO 


trio 
WW 


4»  ft 


o      ^5 


"O         .C  CO  CO  CO  CO 


Is 


is 


ONWH 


■  O  CO  00  00 
CO  i-H  t-  T* 

■>K  00  00 

HIOH 

cOiO  "«i 

COCN 
CO  CO 

1 

CO 

(NCO 

CO  T> 

CO 

tOOCOH 

COCD'O'* 

§ 

CO 

5C 
U0 

i-lOO 

CO  i-C 

"0U0 

865 

887 

922 

1,052 

COCNCN 
00  Tt<  00 
00  050 

CO  Ci 

CO  I- 

i 

00  03 
t-  CO 

ooo 

CO 

oo 

854 

900 

944 

1,049 

§ 

C5 

CTXN 
CO  CO 
OiO 

P3NOK3         •**  ©  rt 
i-l  i-H  CO  t-         CO  i-H  00 


X  —  iO  'O  ©"CO  CO  CM  CO  rfi  no 
»  N  O  00  Ht^H  ©  i-(  ©  HN 
CN  CO  CO  -«ti        CO  CO  lO        IO  CO     <N     co -f 


o    ooom  uo    i-H    o      io  t 

H     WNNh-  COCOCO        O  i 

CO     <M  CO  CO  Tti  IC     iO     CO        Tt<  ■ 


o  o 
o  o 

£■* 

MM 


o  o 

O  O  K. 


WWWh     WWh 


o    £ 


£g  «     '.eh 


*   ^  *  *  ® 


g  8 


©    _^      P* 

©.  F5  ^ 


o 

6 

©       •*-< 


3w 


3£..2£g© 

cc  «2  ©  ^.2.2 


o 

o 

o 

o 

fe 

£ 

£ 

fc 

if 

(J- 

^ 

L^ 

© 

ft 

ft 

ft 

ft 

O 

o 

o 

O 

o 

o 

o 

o 

O 

o 

o 

O 

ft  • 


§ . 

■rt  o 


pq 

PQ 

pq 

pa 

pa 

PQ 

P3 

PQ 

CN 

CO 

id 

CO 

t- 

00 

© 

is 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


399 


C3 

T3JS 

9fl 


oc? 


c 
M 
W 

r 

O  ;© 


o  c  o  o  c  c  o 

OOONOOUJ 


l~  I- 

~  ■ - 

CM  CO 


CO  CO  CO  CO  CO  < 


lOlOlO'fHON'i- 


'O^ONI 


n  01  in  co  t  r  ?  k  t  a:  N  N  K  H  t  ©  C  I  -  -j  X  X  X  « 


i  CN  1"  i.i  N  CO  CO  H 


i  OC  -r  •£  —  ;c  O  'X  < 


i  oe  m  oc  co 


itsoHasoicsMmoHNoiCiCsoccoocoC'K  c 


isssa: 


I'fl'ONH  CM 


'  CO  CO  CO  CO 


■iCtOOO«3( 
NOcomtOc 

CO  ■*  CM  CO  CO  < 


iXt-NHifJiOOHMOCN 
)  CM  00  CM  ^H  ■*  r"     ^ 


381 


ico^xcott-mcSHN^Mcoxt 


T3   O 

co  : 


O  c3  c3 
3£0 


•  rtCM 

•  O  O 

•  O  O 

:££ 

OMJX 

'WW 


•-HCM 

It3t3 

•  O  O 


•  rtCM 


.,-iCM 


'TJ  >>T3t3' 


.  -rT3T3 
.  O  o  o 

•  fto  o 


'tJ'cjtjtj 
?o  O  o  o 


io5M 


•  •  o    •  S>  o    •  51  o    •  £7 o 

•  •  O     '-*  O     ■#  O     ••£  o 

;  ffl  ^  ©  o  ^  ;  .2  ^  ©5  ^  . 

T3  g.JS  go.JST3o.JS  g  o -JS  T3  T3  •;:  .J3  .JS  £  o  •=  •=  -Js  .JS  T3  T3  T3 

:p^h^W  i^w^sa  :  -.pawwpg^www  :  :  : 


J-^  O  O  o  o 

-^^^^  o  o  o 


CO  t»-  OS  ' 


s     £ 


£    £ 


M       M        60        b» 


£^ 


©         CD 

PU        PL, 


O   O   O 

2ZZ 


o    o 


'iflMCN 

6  6 


fl    S 

©      © 


©         ©  ©  ©  3      2 

o       o  o  o  ©  ©    © 

CQ      CCBCQ  PC  CQ    02 


JSjS 

03    03 


)  o  o  o 

r  ©"  ©  ©~  oT  © 
33333 

03    03    03    03    03 

©  ©  ©  ©  © 

pa  pa  pa  pa  pa 


O  O  O  O  O  O  C 


pa 

pa 

pa 

pa 

JS 

o 

JS 

o 

- 

o 

JS    JS 

o  c 

jS 
O 

JS    JS 

O  O 

JS 
O 

JS  JS  JS 

COO 

pa 

•C  T3  jsjsjsjsjsjsjs 
pa  pa  ooooooo 

o 

1-1 

CM 

1-1 

—' 

-1 

£ 

,H 

OC      r-4 

CM 

CO    -* 

<£  l^  OC 

O     «H     CN  CO  t  LO  O  N  oe 

400 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  2: 


•siojiBq— jonpojd  i^t^thi 


180J— q?dop  p3}Oj, 


MS! 


PJ  tT*-^ 


dl3  ^ 
G^OD  O 


ON 


03  O 


fOMMI-N 


•}88j— qjdap  no 


ran^p  8Aoqi3  aprnpiv 


ioooo 


•Gas  A\o]8q     epn^rjiv 


GOOO)HC-l--r--OCOo:l-H(0!DNNOOOI 
1<NOO<N</   -^   r  -r-  CI  S    /    S    /   I  -  /- ■  O  'O  1^  CO  <N  ' 

oooiooiooooo-rpcoTt<-<tirocx)cocot^cooo^-^'*i( 


•;j9aj— 
pa^xjj^anad  ssamioiqj, 


OfNC^OI-   O  ■>'■  "-  ■—  ~Vi-<- 
HNNMNCOCONHCOOO 


OQ-<0 


•;aaj— do;  oq.  q^doa 


NOtiomNNNOniOiOHiPOOHN'q'OOl  ioo«Q  r^i 
[DONii5HOOO®NNNnrt~3iOOHO!Oon  CO  00  OO  CN  Ol 
W^COCftCOCOCXiCOOOC^OCCOOOOOC^CNCOC^Ol  00  <N        00  OS  C<1  **i        05! 


Oh-- 


o  o  o 

ftOft 
e»  >  <D 


o  ft 


5M 


"3  "C  •-*  'C^  *3  .P!  'C  'O  o  h  -Pi  'Cd  "d  -r3 

•.caWm  :  :Wcq  :-  ^Mw  :  :M 


T3    OrM    o 

pq  :Meh 


T3  O 

pa  : 


<N     CO  CO  <N  00  CO  -f 


,5oOtN<Ort<cOt^^H  ^  ^ 

.  666666    6  6  s* 

2  t^i>;^>^>;^^  >~  ft 

J2       <X>    <P    <£>  _C»   <D  _C»     _®  _<D  PJ 

m  ££>£££&  &  £  o 


o  o    o 
oo   o 

ftft  ft 

sa  a 
ss  g 

OD    O 


o  o 


ftft 

as 

d  3 


« 

p 

9 

c 

0 

p 

J 

p 

0 

p 

p 

ooo  ooo    o 

3 333333  3    3 
o  oooooo  o    o 


3     33  3 

02  02  02     02 


S3 

02  02 


(N  <N  CM  CS  CN  CX     <M 


SZ 


a 

o  . 
«  o 

02 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


401 


jo 


©  PC 

08  « 


S   5 

—  o 


1 5 


o  o  v  ie  c  o 


00  t- 

—  go 
s-.  oc 


•  N  uj  cb 


5S 

t-os 


i 


lo  lo  —  ■?  r,  c  i^  u-  -.  rf  c  i-  — 

co!NefflHoo:r-!OCCH' 


co  e«  ■«•  ■<*  o  «o  oo 


BE  oc  —  ifl  t-  iq  — *  tt  l-  l-  —  C  —  re  e  o  S:  t—  ~*  c;  re  r~  u-  cn  CM  cc  cs  (N  -<r  rr 

OCOOi^OCOOOOw^OOcScCC:OcC^0001>c£'--<w.-iOC". 


l-  i-  ci^fic  >.e  l-  si  cc  ~  ■-  s  -  c  ■-  s  c 
i-O  r-  S--  re  i  -  i  -  >  -  i  -  ~  re  oi  ■—  t-  re  co  o\  s~~  io 
tiL^N  oooOfo-*,lOt~oc-r■^,^e^o■^lce^?■^< 


WMCOM10tt*l010»0«t*00'-IM  — 
■   —  0C  COOOCMM  ' 

OOOOfO'^'^'OOOOTJi^roOl 


OC'  O  ob  m  y.  l-  c 


-es  or  oc  t~-  Tf  oc  i 


OC  CCTTCOI 


u-  l^  a>  cocao  ic  >e  as  to  ©  u-  ua  c 

S  o  n  c  /.  c  z  c  m  c  ■-  ~  e  - 

«ONNNX«CNNX'/.'Xt- 


N  N  -  c  /.  O  r:  C  C  C  -  i  -  -  N  C  l^  n  -.  c  r:  C  C  -  «  M  C  Z  M  C  C  -  !S  c 
-i  ^  C  C  ■-  ~  rt  '/-  -  N  t>  ~  C  -  c^  -  ■;  C   -  -  1-  -  '/  M  t-  C  -  -  N  e  C  ^-  N 

r.  n  r:  t-  -.  x  in  n  -  z  «  i-  ~  as  N  re  ue  ob  cq  x  oc  en  cc  N  n  at  w  x  oc  85  c^  oc  oc 


C    .73  s- 

a  'oft 


•73  J-     -73  jr 
•  o  c    .  c  c 

'Cft     •  C  ft 

;    >  ©    •  :>  © 

or  co  **"  oc    •     •  cc        0£    •  ^  OJC    •     ■ 

"Ocj-^'doccj-'sc^'coc 


11-KN 

^7373' 

5   C 

a  c 
•5  ? 


pS?M5 


:M«  :  :^^ 


- 

3 
C 

pa  :Wi 


•73  £73 
■  C   O  o 

•  c  CC 

=111 


»->     •  C73  «- 

O      .  c8   O  O 

ft  •  n  c  ft 
73  0-0^73  o 


cc 


re    <N    <N 


S3      e8    £    S      £ 


ei 


s  s 


CCO  OOO  00 ^^  L^  ^ 

£  Iz;  £  £     £     £  £  £     ■  ^  „•       ;  j     •       J     ■       :       !  00   -:  n  ^  o 

§§§  =     §    5  =   §   c    c    d      ceo      60      6      6oZZ  Z  Z 

www  www  wwfcfcfcfcfcfcZfcfcfcfcfto,  ft  ft 

ft   ft  ft  a     ft     ft  &   &  ,_.-  „_r  _r    _r  _r  ^-     ,_.-  _r    _r    ._.-,_,-£  p,  2  £ 

Sec  c      2      2  2    2  "©   "©   "©     '©'©'©     '©"©"©'©"©   J3J3  2  J3 

tni.nSH  52.2,2J.§,2,2i2,2,2i2i2«8«a  S  cs 

OOO  OOO  uqS22     2232Hu;HC2  jj  J  J 


g 

= 

e 

e 

jj 

e 

■ 

C3 

e3 

I 

<S 

e 

e 

e 

a 

e 

e 

01 

QQ 

CC 

EG 

QQ 

GO 

c    c 


.2    °  .£ 
!c  2  S 


— 1     CS     CO 


■*      10      so 


-26  G 


402 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spjjBq— jonpojd  i«iitui 


•jaa;— todap  ibjoj, 


•}88j— qjdap  no 


t3 

CD 

a 

a 
o 
g 

I 


I. 

53 

o 


•^88J— 8UBld 

ran;ep  eAoqe  apnmiv 


•^88J— 18A81 

B8S    Avopq    epn^i^v 


•}88J— 


•j88j— do;  o%  qidaa 


3  £ *  £ Q® 


"CCS 


HOOHOOOffltOOHOWON 


t-  CO  CO  CO  CM  io  <N  50  <M  CD  IO  00  <N  CO  I— 
CO-<cP-*'CO'Cfi-*HO»000'^lCO-W|iOiOI>- 


OWHNiOOiOOOIN      •COiOOJCO 
NHCOlNlNIMrtOi'^CC      -CO        t»i 


lONnioioiooMOOioooowc 
— ■  -  ■  s  hi>o,/h  r  -m  /-  .m  .-  cr  ■— 
OOOOOOOC00050iO(Nc3it-CT>05a><M 


flT3  J- 
Pi  o  ft 

§  fe  s. 
.OS6*5*    •    -.a  cr 

OOOOOor^T)OOOoC« 

Td  t>  t3  t3  t3  a  •-<  ■£  ^  i3  T3  3  O 

:  :  :  :  :pqWpq  :  :  :pq- 


;  id1 

"no 


OC  N  N  H  (N  O  <N  IM        O  CD 

r-HCOOO(McOCOt^-CO        OU5 
<-H  o  OS  <-H  O  O  O  O         IO  CO 


OJiOOOIOOOOh 


Ml 

TJOOOOOOO 


o 
o 

-si 


*    6 


NCCHTf 

6  6  6  6 


M)       6j0 


O  O  O 

&  && 

T3  "dT3    .2  2.2.2.2 

■g  -c  'C     &  ia  rd  is  ^i 


££ 


O    CQ 

pa 

pa 

pq 

PQ 

m 

P2 

PQPQ 

ooooo 

CO     CO 

CO 

CO 

00 
CO 

03 

CO 

o 

"* 

CM  CO 

rt  CJ  CO  ■*  ^H 

4* 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


403 


His 
mm 


Od  <Ow* 


33: 


oo 

COCO 


oo^iooooit-coi— icocor^t-~iocoo"*>t^cocooooococ^O'<J1coco 


O  O  iO  O  CO  00  ^H  00 
HIMINiO  O  NHTt< 
HO0C»     CO     (Offlffl 


00        WWOOIOOOON 
■*       OOO00ffl>0«NN 


loomMNOoiiiNioooo^o^ioH 

|'*OOOCO)OCO'*0(ONOOOO)OOCO'* 


CO  CO  N«0»NV 


00«50  00  CO  Ci  t- 
05  CC  Is-  io  o>  t^-  00  lO 
COTPCOOO     00     00  00  00 


i  Tf  ic  t-  oc  as  i 


ootOH^rtNioocs'oiooocicooMOiooNmiNMMtcoooo 

HNM        *HHtjiu50        CO        rtrtrtWrtHMHOOrt        CO        CO 


O  O  00      CO      lO  CO  i 


lONiN^MOHOHioooNm^nowooo 


lO  i-l  00  "*  lO  CO 
.  .  O  i-l  00  Oi  CO  CO 
t^OOOOCii-lCOCOOOTtiTfi 


WlOOO      CO     CO  < 


co      oooowooooc 

CO         HNOMNOCOt-Ol 

Tf      as  oo  o  i-i  co  co  io  co  co 


'S&'g'g-'g 


..-d-d 
ao  O 


id-*.* 


d 

_  o 
o  o 


.-d-d 
i  o  o 
i  o  o 


•"•d-d 

•  o  o 

•  o  o 


'd-d  p  £C!---~  S'd^dd  s^i.isjs  g 


b  :  d  •" 

T) 

c 

ft  •  p   • 

o 

CD      •  C3~ 
M    i^  en 

* 

« 

'CSSO 

.p 

«  :cq^ 

M 

T-H(N 

ni'i'd 

o  o  o 
o  o  o 
£££ 


!   ;  *>i  co' 

•              (-4 

o 
'     Pi 

1 

p 

l;M 

CD 

?    -d  c 

c 

j     •g'd'd  ptt-S  S  o  o 

;  m 

PQ5: 

ME-S3K 

ICO     V        CO 


oocoio    i-i 

CO 

£ 

o  o  o    o 

o 

■d 

Skiles, 
Skiles, 
Skiles, 

Skiles, 

_© 

CO 

o 

o    o  o  o  o  o  o 


•d  -ddddd*d  *d 
o  oooooo  o 
ooooooo      o 

£  ££^££  £ 


o  o  o    o 

332  3 


o  oooooo  o 

On  On  P<  O-i  Ph  P-i  Pt  Pi 

CD  CD  CD   CD  CD  CD  CD  © 

bO  cuObCWJbCfcJDW)  tuO 


ooo  o 

o 

pq 

n 

CQ 

P3 

CQ  pqpqpqpqpqpq 

pq 

PQ 

CO  00  -v     iO 

CO 

00 

CT> 

o 

^    co  co  Ttt  m  co  t- 

00 

OS 

404 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spaj'Bq— ipnpoid  iBprai 


•^98j— q;d9p  \v%o £ 


laa;— mdap  no 


tani'Bp  eAoqc  opn^piv 


•%99}— I8A9J 

B9S  JAO\aq     apn^piv 


pajEJ^twd  ssau^otqj, 


•}38j— doj  o;  tndaa 


3s'3 


©HtONOONOl^MN^VOCONfflfflHOOiOOniniflNOOCCWI 

■*i-iM'*wa3Tt<OLO'*ininiocoN'*MOciCHoai(Noi,(NaNo>'*( 
ooHtoHooooioooHHOooioJNeeiooHooNffliooi 


HO)tcOCOrJOrtfflNOCW!DONW*HO)NlOOMniONO! 


oocyte 


rH  CO  10  <N  <N  O*  <M      .HHtDNNNOONOHH       (MNMOOhhhNhN 


t^-  i-H  O  t~-  i— I  <_ 

C»0500C<)OOOOlM050500bOOOS.OOOOOOOO'^COCOCOOiCOOCOrHCOCOo605 


JCOOOt'lNNCOO^OC^HOJNinCNiOiCNCOHNOO 

1  co  r 


o  o 

O  ft 

RSm    ■  j 

£-3  o  o  o  o 


HNM     • 

c3     .  o  O  O  © 

a   '  o  o  o  ft 

.s^e^s  .  . 

ooooooooo  c?  ^  ^'doo 

T-ln-!iT-trr-(n-|rr-!'r-(tT-!  r-t   t- .H  _*-!.'-!•— it-(it-I 


■£"OOOOOOOOOOOOOo  w-, 

,^-^x)T3,rJT)'0'i3'C'c!rdT3'C'Osi3.i:.^.!5-C'c( 

Wcq  :::::::::::  :pqa2WMWPQ  : 


o  eg 

PQPQM 


O  ft 
P  be 
£-d  o 

Mm  : 


3  2.2  £  S  ® 


525     fc     £ 


o      o  o  o 


&££ 


0 

O 

o 

O 

o  o  o 

O 

ft 

A 

& 

ft 

ft 

£ 

c 

w 

W 

Ml 

T3 

>d 

T3 

-d 

'CT3T3 

>g 

ft  • 

03  O 


S     . 

53  o 

8* 


CQ      P3      P3 


pa    papapa 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


405 


(V  o 


oomoi 
*a<  t~-  i— i 

co  oo  a> 


OJNN         MNnOSTN-TI r   X  '  C    M  "5  CO  N  OS  M    X   CC  00  CO 

OOOOi        ©OO  OOOO  COOOOO—<00  rt  O  <-h  OOOCO 


Ci  CN  -*<  Tt<  *!}<  t--  ( 


D  CN  CT>  CN  CO     -<Ji     C 


co    os  co  zoin id  i-H ct> os ^ co  t» 


CO!OlOlOHO>OJHCONi*Tll 

S->*ii-ico-*f|r^^cocor—  cooo 
Ot-HOOi-iOOOOTPCO 


CO  iO  CN  r-         tONCMt-MMAWWH 

^^  ^  iC      00TfTft-'^TF'<cP*'ch00'^,'cti 


o»nhoo  as  cm  cjs  >0  t^  cn  3s  i>  i-  eo  so  -r 


•O  co  -r 


Tf  t>.  Oi  O  ■*  Oi      o>     CO  ■*  ■*  CO  - 


■  O  O  OiONO-C'-CCiSXHtONXL'rOOOlOOO 
00  CO  NNHMHOCINOOOOOOHOHOTOSTrKTPW 
00  O        CO  00  C5  00  OS  00  OS  CO  00  CT>  00  00  00  00  oa  i  OC  OC  I  -  CO  OO  00  lO 


ICO^POOCO     CO     t-  00  00  00  00  00  t-  00  Ol  00  CO  ■*  >o 


13  O  O  cj 

pq  :  :cq 


o  © 
o  ft 

£!t3  O  O 

W.m  :  : 


O    O    Or«' 


£  3 

T3^ 


i-HCN 

5  fi  li -C)  "E  T) 

5soo2o 
PkO  o  o  &o 


-OOOOOOOOO 

fnMcePPfqMWfqW  w  pq  :::::::  : 


T>. ft 


S5       S 


„.  S  B        00           *           W        S           *           « 

6  6  66666665 

c/T  t/T  oT      oT        of        m"       si"         m          k        ^ 

©  CO  ©CDcDfflCDOCDo 


0 

o 

o 

a 

£ 

fc 

|Zi 

fc 

,c 

fl 

,fi 

,Q 

0 

0 

a 

a 

o 

o 

o 

o 

u 

U 

o 

U 

M      "C       #c 


pc 

ffl 

C3 

pq 

PO 

CO 

22 

CO 

pa 

m 

02    02 

DQ 

02 

GO 

02 

02 

02 

02 

CN 

CO 

o> 

o 

CN 

8     83 

■  CN 

CN 

8 

CN 

00 
CN 

8 

O 
CO 

406 


OIL  FIELDS  OF  CKAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spjJBq— pnpoad  i^piui 


•399;— q^dgp  ve^o  j, 


•^ggj— q^dgp  no 


CO 

O 


•199J— gtrejd 
rarnep  9Aoqi3  gpnmjv 


199J— I8A9I 

B9S   A\0|9q   gpn^iv 


•}99J— 

pg^J^gugd  ssgujpiqj, 


199J— do;  o;  q;d9Q 


£§i«S9> 


MONiOOtO 
iOO 


g§: 


12^ 


-d-d 
o  o 
o  o 


t3  o 
■CO 

pq  : 


§2 


ratf 


£8 


-J 

•a-2® 

03       Ph 


(OrtHHlOO5HT)((DNlO00         OS  ( 

(OC<HOrtO>»00tOMtDINO)        «H  < 
OOOOOOujiOOOOOiS        CO< 


'  io  w  a -^  <d  o  to  oo  ■* 


Tji  Tf*  ^  Tf*  CD  05  Oi  "^   ^J1   ' 


-^■^oooooo-^-^-^-^tji. 


N1O00NCOHIONH 

ItHiON        CO  <N -*t>  i-H  <N 


cONCJOONiONNNMN- 
lOWtOHCONHHHN         ( 


NNNOO!OH( 


OOOOOOJOCOCOOOOOOO)© 


I  CO  00  05  00  OS  00  < 


0300° 
f3  o  o  ft 

'dooo'S^'Ooooo 

'£ro,&ro  0 .J3 .Jh *e 'C ^  tz> ^ 
pq  :  :  :pqMMpq 


O  .-h 


) 

oc 

<N 

<M 

<N 

oa 

CO 

>H 

lO 

O 

o 

0 

o 

o 

O 

O 

o 

o 

O 

o 

£ 

fc 

!? 

fe 

£ 

fc 

fe 

fe 

|Zi 

£ 

£ 

43 

45 

43 

A 

43 

A 

43 

43 

43 

A 

43 

3 

a 

a 

a 

a 

a 

a 

a 

a 

s 

a 

CO 

02 

CO 

CO 

DO 

TO 

CO 

CO 

CO 

CD 

CO 

sz 


ft 

ft 

ft 

ft 

ft 

ft 

ft 

ft 

ft 

ft 

ft 

OT 

Ki 

en 

to 

i 

a> 

$ 

3 

® 

9 

© 

jy 

3 

a 

^3 

53 

^3 

^3 

!9 

zi 

a 

^3 

o 

o 

o 

O 

o 

o 

o 

0 

O 

CJ 

O 

fc 

1? 

1? 

£ 

fc 

fe 

fe 

£ 

£ 

£ 

fc 

H 

w 

w 

w 

H 

w 

s 

H 

w 

w 

W 

00 

o> 

r> 

CO 

CO 

CO 

CO 

•      CO 

CO 

CO 

CO 

BLATCHLET] 


TABLES    OF    WELL   DATA. 


407 


3 

a 
It 

"3 
a: 

§ 

CO 

C3 

© 

g 
■<»< 
OS 

a  a 

S"S 

3  r. 

X  X 

- 
- 

* 

— 
r 
X 

'3 
•a 

1 

- 
— 

- 
- 

£ 

X 

| 

P 

CJ 

c 

- 

s 

- 
o 

- 
a 

o 

s 

CO 

T5 
c3 

IQ 

N 

,2 

_   S 

g-2 

•a  : 

©  . 

=  • 

o    • 

-   : 

a   . 

03  • 
,C     ! 

e8    : 

~z 

I- 

OB 

— 
r 
X 

- 

£ 

- 

1 

u 
a 

r 
X 

X 

d  o 

—  — 

z 
I- 

= 

gg 

= 

M 

c 

- 

r 
X 

©    ! 

«2    ' 

S  : 

CO      • 

S  d  3 

III 

I§1 

- 
.J. 

re 

£ 

CO 

— 
-2 

IQ 

IQ 

o  o 
mm 

o 

CO 
r^co 

S3 

o  ■ 
■a 

|  : 

5 

LO 

s 

X 

— 
re 

1 

OS 

00 

lO 

1 

•v 

— 

to 
■a 

CO 

— 

a 

r — - 

oto 

C5  C5 

OS 

o 

OS 

1 

CO 

— 
X 

OOOfflOil^wOCr.CCMOCKi-' 

CO  re  l-  ■ ■-  co  OS  00 
—  CO  X  CJ  —  i  — 

moooociso 

t-OO M  =  •  -  '  -  C  C  C  -  it  C.  O  00       MNNffliafflrttM 

CNN        to  C^  —  CO  to  —  rc-.il- ~l:  ■-  Oi        u-t— '  [^  CO  O  O  -*  t~  CO 

CO  — h        OCXOrr--  —  ©s  ie  — •  uO  CM        XXX^iO-fClcOOC 

t^  r^      cooiooeoiotoeoeqiocomeoo      —  x  oj  o  ~  co  x  cs  c- 

tt  as      -s-  l-  tt  i_e  l-  so  oo  l-  r-  op  cm  lo  r-  o      orr«oir.Nosoc 

t^  <N  O  CC  O  OC  l-  u-  ~  —  OiCXL-rr-  C:  "  -  C:  ^  CO 
CN  <M  CM  ^r         CthNhNN               XVHNN1--ON 

■  co  -<r       co  co 

OO                CO 

OllflOTL'tNOCSCX         CNCCCCC^CX 

IflOMNOOlCONXNrL-N-.  NCOOCNOVN 

SOcQNoen«ooioocQ(oooo'«oo«oa<DH 

X  CO         —  —  —  "O  CO  CO  CO  O  CO  lO  —  CO  CO  t^         MOOMHlOOlON-fl 

—  ~ .        "O  re  X  d  3COO>»iOWONNM        Xri X  CO  l~  X 

X  re        X  CO  X  CT.  O-  CO  CO  CT.  —  CO  t-  ©.  — '  —        —  ©SCSTrrrcC^rT-c 

1 

- 

- 

c 

c 

- 

>  c 

C 

c 
- 

- 
C 
C 

| 

5 

1 

| 

3 

!  c 

: 

: 

c 

7 

c 

c 
c 
« 

\\ 

j  = 

;- 

- 
c 
z 

s 

_ 

5 

1 

1 

■ 
c  . 

D    C 

: 

r 

1 

: 

0 

•  a 
■  t 

.1 
1 

) 

C 

c 
B 

z  c 

— - 

c 

1    C 
|  c 

-r  i 

1 1 
i  i 

c 

|  : 

-=  : 

>j5  = 

:  j 

;        1 

'    Q 

i  is 

-    '  : 

h 

3  ^ 

I 

> 
) 

C  o    ■    •  c  c     .    .  o 

^  a  ..  .  §  a  •    ■  o 
fzz    :  oq  M  ffl  oq   i  M 

CC 

t^ 

CN 

— 

CI 

o      o  o    o 


©  ©  ©  © 

ft  p,  'E'E 

in  m  to  co 

O  ©  ©  © 


a    vO  a 

CO        rtN     M 


408 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


*o    • 

CD 

:  !  ca 

CO 

M 

C3 

•  a>  co 
:     <2ota 

:    §3J5 

£  : 

o    . 

a  : 

a" 

O 

:  :3 

:  ;  o 

a 

00rH,-l 

O 

:  :fc 

* 

(-T  tT  ^T 

co  co  co 

(-1  "co 

b 

■IT5      ■      -CO      ■ 

;  2J>    "c3"e3"§ 

-a 

:  ':! 

•lO      •      '»«      • 

:|    £  £  £ 

££ 

-2 

"  ;  !rH~  ; 

§ 

■       •   CO 

•  CO        •       'CO        • 

•  03     ■     •  c3     • 

•  R       CQCOCO 

CO 

3 

:  :o 

:o  :  :o  : 

: 

3 

>> 

-*  — 

•  iO     • 

O  '" 

:g 

co  o  O     •  O  i.O  o 
esco  00     •  lO  CN  CN 

•siaxreq— ;onpojd  p3i:nui 

e 

o    - 

. 

-- 

c 

CN  00      • 

,679 
,532 

"550 
,569 

•^88j— mdap  i^ioj, 

: 

c^ 

<5 

Sri 

'S    '»o 

-Hr- 

;rH      .rH 

.       .rHrH 

• 

o 

"3        1 

x  -- 

•;88j— q^dap  no 

OS         CO 

re  y 

"fM^TT 

>o  "0 

CO  lO  -rJ<  lO  »C  ITS 

1-1 

H  "" 

;HHr"" 

HH 

rH  rH  1-1  rH  1-H  rH 

•}88j— au'Bid 

ON 

c  o>ooo      O"- 
co  CN  co  O  co      os  r- 

t^  CN  OS  t> 

CN  OS  CD  rH 

OOt»^»HM(iJOMC 

CD  lO  CD  CD 

HOSt>^M           r-(      | 

tOiOiCOtOLOiOiC^W^t 

CN  "3<  -W  •*  •^  rr 

turnip  SAoqc  apn^Tiiv 

~ 

'd 

COCN 

OOU5C 

O       co  »o       CO  OC 

OSt^t^Or~0-*lO-rJ<-^" 

& 

•}88J— I8A8I 

88 

I—         rH  rH         NOMCCWONXS'nCBiOCr.NMrHaoCN 

i-i      co  »o      oo  as  os  oo  oo  as  as  as  o  o  o  o  o  cn  o  o  o  o  o 

.    ess    Avoiaq    epnjT^iv 

-\T 

VT     t-T- 

-t-> 
a 

•^88J— 

S§5 

i-l  CN 

2      8 

oooot^o 

CN        COO 

otoioc 

CNCNr-tCN 

O  CN  CO  CN  TJ<  I> 
CNCN           rHrHr- 

i-O  t^  CN  CO 
rHCNCN 

o 
O 

t3 

pa^jjauad  ssau-qoiqj, 

COiO 

OOiOC 
O  rH  CO  CO 

OOOHC 

O       Oir 

l>  CN  id  OS  Ifl  I"  K5  W  t  - 

CNOLDOOIOIOOSOCOCD 

O       "»<  -rj 

OTfOr 

cc  5 

■*OHH 

i 

CO 

•^88j— do;  oi  tndaci 

CD        t^  O 

CO  CO  CO  60  W  ^  CO  -^  M- 

to  m  -*r  «: 

-tfi  lO  lO  lO 

co 

S 

o 
Eh 

:  r 

CN 

•       ;r-ICN 

rHCN  rHCN 

• 

1 

o 

'h 

> 

^ 

•c5 

,'CdT3rOrc3r6rCJ'C 

■  c 

•  o 

Pi 

r.  C 

o 

o 

'  c 

'  o 

£S 

CO 

^£ 

£      ^c 

\> 

»J2  2 

:^^^^^^^^ 

fe?& 

io^ 

w 

■as 

•3       gc 

oij^iipi!^^^^  o^ 

C3-«     O    O 

1 

Oh 

i)0«J 

'-.- 

O-tSTS'O 

Sa 

«    :rW 

M    eh£ 

z  g 

M^ 

:WWM«w^wmh^ 

^W  :  : 

1 

iO     OilN 

5Sj 

Sur- 
face 
ele- 
va- 
tion- 
feet. 

c 

D 

•* 

CD 

rH           CN       CO 

CO             OC 

IC 

£ 

^ 

i«        us     « 

co        co      a- 

CO     CN  rf< 

TT      T 

CP 

TJ1            "tf       TT 

^*i        ■* 

icf      TT  TJ1 

o 

O 

<w 

o 

1 

O     CO  lO 

rH      CN 

•<* 

c 

C 

6      6c 

6    6  6 

o 

O       C 

c 

^ 

55 

^     ^ 

Z      rZrZ 

^ 

.    I 

r" 

D 

5 

cu 
P 

.a 

)    b2       bo    bi 

.a  .s  .a 

;  o       c 

"Z             rZ 

c 

rZ 

bo    bo  bo 

a  a  a 

fe 

co     cr 

©    a 

SB 

M 

i^ 

www 

CO                V 

C3           <S 

- 

W  WW 

■1 

> 

»  > 

,>>>>> 

0     >>     >>>> 

3 

H                 tH            J- 

3        E 
o        c 

c 

•  g     -  - 

CO       CO   <» 

P    O 

r 

> 

Ph 

PM 

H          H      H 

ft       P 

p 

Ph    PhP-i 

>> 

A 

a 

o 

3 

o 

p 

M 

Q 

o 

3 

B 

a 

C3 

* 

o    c 

c 

0 

o      o    o 

o        c 

o 

o    o  o 

fe 

-=:    .c 

2 

^3 

A 

rC            r3       rC 

rC3              rfl 

rC 

A    AA 

O   C 

E 

3 

O 

Z 

o    o  o 

O              O 

0 

O   OO 

O      rH 

,— i 

a 

CO           ■*>       l-H 

CN           CO 

-r 

iO     CO  t- 

&d 

2£ 

33  o 

H 

F 

3 

w 

£ 

CO 

Jl- 

1 

CO 

5 

J, 

z 

^z 

BLATCHLEY] 


TABLES    OF    WELL   DATA. 


409 


o     o.£ 


03  M 
£.5 


oqO 


m     m 


8  :S 


l  00  lO 


t>  co  coco  o 

lO  ■*  -V  rr  tf 


S3! 


I^CO^Ht^t^cNcNt^-t^t^cNlcNC^r^ 

^^  •oooo-*oor^<Nt^<Ncoi>'a< 


lO  CO  t^(M  , 


O    lO  00  CO  t~-  Oi  CO  t~-  05  CO  CO  00  00  CO  CO  CO  00  00  CO  CO 

oo      oor~co-*'t^com<Mrt>-iiococNc^eMr~~-'i..- 

iO       NOlOOOHHNMiOiOSONXlOOOOlOO 


O  CD  CO  CO 

-TC   T-H  CD  t- 

TPiOcOO 


•^  CO         ff 


)  ooo  co< 


iOHNNCOMtPOI 


m 


°  M  ° 

.a  o.a 


o  a 

do 


.-H<N>-iCN 

o  o  o  o  o 
o  o  o  o  o 

£££££ 

.a.S  .a  .a  .a 

k>kyl  kyl  k>  kJ 

-£.  >2£|  pC|  \Xi  — 


•*-    03 

■  fc  a 


<N03      •     ■     • 


•  d  dd 

'OOO 
O  O  O  ^ 


*ft 


!dddd|    -ga^-g-g^gG-od 


N 


i  M 


T3d 

m  :  :m 


o  o  o  o 
dd-d  a 

:  :  :m 


o  o 
o  o 

O  C3  c3  ^  ^ 

a  ho---s 

W022    MM 


<*i  tp      CO      NMiH 

•fioood    6    odd 

£h  £<  tJDbJBtuO    b2    tJObCbio 

..-gag  g  g  a  a 

11'mmm  m  wmm 


N 

w 

o  o 

d 

fci< 

fc 

fc 

aT 

a? 

co  en 

ft 

ft 

•d-d 

ft 

& 

raaa 

£ 

(0 

^3^5 

- 

- 

OO 

mm 


•d 

-d 

d-d 

£ 

£ 

££ 

o 

o 

o  o 

a 

a 

a  a 

02 

CQ 

mm 

ooo  o  ooo 

222  2  222 
ooo  o  ooo 


o 

O 

CO    CO 

O  O 

pq 

m 

mm 

a 

a 

a  a 

<e 

CC    CD 

d 

— 

dd 

* 

* 

££ 

o 

o 

o  o 

a 

a 

a  a 

00 

ou 

mm 

.1* 


410 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•s-pxreq— pnpojd  i«prai 


•}88j— q^dap  \vio  j, 


•;88j— mdep  no 


•^88J— 9UBld 

rarnep  aAoqB  9pn;i^y 


'188J — pA9] 

eas    Mopq    epn^mv 


•199J— 

pe^jaouad  ssau^oiqj, 


2£ 


dqH 


',2    *H  ■ 

1       o 

>CO    O 


|.H    O' 


t^OUJHOOO         HlOO)MONCOlOt> 
HOOOJOOOO        l>-  CO  Tf  tji  -sr  CO  CO  <N 


>  tT  iO  iO  CO  CO        t^WOOOHHNv 


oifliooou)      LoowoNanoo) 

NN         i-H  <N  i-H        CO  i-H  i-l  i— l  <M        i-H        i-H 


•?88j— doq.  o;  q^dea 


O  c3  fl" 

«  >  2. 


C3  O 


oiomiooo 

ONNOOiN 

ooaoooH 


JONOfNO 


CJO 

id  o  o 

pq  :  : 


o  o  o 
'drdT3 


™  «-  o  o  o 

d  fl  o  o  o 

C3  &£££ 


m  3  .S  .3 .3  jh  £  o  T3 


9hO 


tx. 


g?33 


383 

«o>o© 


igjCDCD-^i-rfOO-^OOC^OSC 


NOOtONNIfNffllOHHOH'* 
OmOCO-*lOlOHlOHNHO)i-l 
i-Hi-h<MOOOCTiOO<M,OCNO(M 


uO  CD  O  i 
T<  T  O  ' 


;oocmo5io-^coooc50co 

.^0<NCOCOC005<M  cocoes  -3- 


o  o  o  o 
o  o  fto 
tefe"- 


^h    oo    nhioio    oo    oo <35    oj    oi oi 

t^     O     O1O5O500     t-     CCM     CM     <M  <M 


U0! 

-r      -6 
p<      ft   ») 

<?    ®  a 


J^  lO  i-h  <M     CO 

-6  6  6    6 
|££!z;  &  55  6 


o  o 


im  Id    03 

HCCOJC0CQ    COO    O    Hh 


<55'o'oro 


pq  PQ 
a   fl 


-d  T3 

^  ^.2.2.2 

JH  rl^H^H^H        A        ^H 

02  i»000   O   OO   O   OO 


o    o 


o. 


M     M     OO 

22 


N     H     INW 


»0      CO      l~-  i-H      CM      COtJi 


[bull.  no.  22 


TABLES    OF    WELL   DATA. 


411 


©  ©  O   © 

.2 .2 -5 .2 

hco  c3o 


OO^O 


WON 


en  o  en 

COO 


#CM 


EhO 


'po 


«  '§88  8 


mooujo 

t^  CO  LO  C^  CO 


CM  00  t-  iO  -*i  t>-  L?»0> 


>,icm 


H00 

CO  LO 
CO  00 


NWNO 
■<ti  lO  CO  -* 
COcOiOiO 


j  CO  CO  CO  CO 


(N  CO  CO  N  00  lO  rt  ■* 
COCOCOOO^t^COt^ 

cococococococ-co 


ss 


00  CM      ■  LO  CM 


OOCN 
^h  00  CO 
CO  CO  CO 


OONHOOOeHHOl^MCOiOHOOiQCNINNOOOOOOHHINiONHiOiOiONOOOHIMcNOi 
ajOOiOCOCSMMWmCSpCOHOCOC^^MNNNcpCJHNCON^CNMmiOcNOi   — 


ICO-^CO^-<TiCO-^COCO' 


'•^CO-*lCO-*,CO-*iCO-*'CO'*iCOCOCOI 


CSiOiO 

CO  CO  Oi 

CO  CO  CO 


CM  00  OiO  O  O  ' 


iC»HCDNNl0C»(NlO0000C<5'*OCNC<10>a)00lOC0anOl0WMOIN< 


CNNOHNONNOI 


00OTt«Tf00ON(N 
OONSOOHOH 
HOrtNINCNCNIN 


oo  io  io  o  cm  o  o  co  o  r^  oo  o  io    'iflTfOco    •nconnoco    •  cm  cm  oi  oo  io  i>-  t--  oo  co  i— i  co    >i*-    ■oiooukduj 

i-l    T  i-l    i-l  CM  i-l  CO  CM  rH  CM  CM   .  -tfi  •*  lO  -cH   •  CM  CM  iO  CO  r-t  i-H   ■  CO  CO  CO    'fl'HH^HINlM   -CM   •  CO  CO  CM  CM  i-(  CM 


NlOC0OOO<*0)inN-Siini0WM(DI)0HlOOCN00OONN!0WHNMMC0IN00OM0(0CDOOOl0IN( 

'VfNM-O'Ot'J'OMMONWOONOHHHNHNHOHOlHr- 

cOCO'^f,lOCOtOCOCOlOCOCO»OcOlOlOcO 


iiOiO-'cHCOiOcOiOCO^cOiOcO^fCOcOcOcocOifco-cncOcOcocOcOCO 


OOCN  CO 

CO  t-  Tfl 

lO  kO  »o 


.^M    ,M 


:  t>>>> 

r«        -MM         ■ 


0  0ocqOq0oqoooSoo2oo2oooSoSo2oSoSoo 


>>  :  >> 

.^    .  ^ 

>>n  >>c? 

©2  ©2 

>  go  2o  o 

:HSe§  : 


00         00         00         00 
CO         CO         CO         CO 


-1  O  O 
gcBc^SS 


CO     i-l     CM 


fc   £   £ 


^6  d£ 


£  fc  £ 


£  £  £  £ 


.3  .3  .3  .3   s  rt  ~ 

o    o    o    o    K    E    s 

O   O   O   O   O   O   £ 


44|  1 1 1 1 1  £  jfii 


42    +2.£cH    i-' 

s    s  s  ©  ,■ 


£    P 


"2  ;5'5'5.2H  .^ 

S       &  ft  P<£3      ^H 

eg  P^pm  m 


^     ^     ^     ^     ji  c/jododrt  P?     S 


i-l  CM  o 

6  6^ 

£  fcfl- 

..  .,  o 


HU3d66 

^  ^H    ©    ©    © 

o  o'ti'O'd 
W  OT  &&,&, 

oo    •    •    • 


£  o  o 
is©'"^"' 


o  o  o  o  o 


.2  £  2  -2  2  2 
a'aaaa  2  2  «  S  3  3  2 
ooooo  o  o  S  o  o  o  o 


lOCDt^OOCi     O     i-l     i-l     CM     CO     ■"*<     i-l        CM     CO  •«*'  to 


o  o 

r  r 

2  .2>>>>2  .2 

^)    ^oScS^    A 

O  OWWO  o 


o  o  o 
o  o  o 

o  .2.2.2.2  *** 

A    AAAA&G& 

o  ooooWWW 


AAA 
ooo 


l  CM  CO" 


IC 


t^  00  OS  O  i-1  CM  CO        i-l  CM  CO 


X* 


412 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


o 
o 

a 


•sjajxeq — ^onpcud  ibi^tui 


•^aaj— i^dap  p^oj, 


•}98j— q^dap  no 


•^aaj— atrefd 
ranjcp  8AoqB  epn^py 


•}88J— \3AQ\ 

B9S    Aiojeq    eprvjrnv 


pe^Bnenad  ssan^oiqj, 


•^88j— doj  oj  q^daa 


£S©. 


3  ^~  *  s 


u 


O  03 


!*-§. 


O2P3o2  0Q 


§8 

coco 


23 


02O 


00  O  <N  00  t- 

«3O0O0t^t- 
COiOiOiOiC 


CO  i— I 


»5 
05  £ 


pq 


COCO'-tf'COCOCOOlCOCOCOCOCOCOCO 


iO  CO        ©  C 


I  (M  ,_|  ,_|  ,_|  ,_,  I-H  , 


©io©oo 

©C^iO  ^ 

io  t^  oo© 


OO^OrroiOiOO^OOOOCN' 

t-  t-  ©  ©  c-  (     - 


0!iflt-0)0)  ©  tH  CO  ' 


>  ©.2.5    .  ©  t>>.2  ; 

^«oo°S So  2  o  O  O 

w£^S  :&£Sh  :  :  : 


©  ter 

•IS 


O  o  o 

OP  fe.  © 
bOp*  bO 
TJf^TJ  O  O 

wWw  :  : 


oo  r^  rti    io    ©    © 

COCO  CO     CO     CO     CO 


r~  io  ©  © 


o    o 


6oo    tT  J  h 

£££    §    §    6 

5  as  II* 

•S JJ    of   oa°  .2 

I  a  a  ^  *=  S 


o  o  o  o 


aaaa 

03    ©    ©   © 


Jj+J+J  ® 


H<1^    OOPN         fin      MMME4 


o  o  o 

O  O  O 

M  M  M 

.a  .a  .s 

a  a  a 

=a  «  « 

©  ©  © 

P5  P?  tf 


2  2  2 
333 


SIS 


ci   a   pi 

O)       ©       © 

OOP  oou 

HHIN      CO      fi      lO 


+3         O  O  O  O 


Q    oooo 

©        i— I  <N  CO  •& 


©£ 
©^ 

02 


I  Bad 


BLATCHLEY] 


TABLES    OF    WELL   DATA. 


413 


'.* 

s  • 

£ 

;  (■ 

8 

it 

Sot 
o  p 

ft 

H      ■ 

J4 

c 

« 

is 

03 

<£ 
io 

P 

'+3 

03 

<s 

00 

s 

"o3 

11 

I'd  03 

B   .M 
o-d-H 

I 

0 

CO 
re 

i 

!© 

03  _ 

CD  i-H 

0^ 

Cs3 

.a 

•   4 

>  a 

:§ 

!  p 

!  a 
■^: 
■  sr 

; 

JB 

!  bo 

:.S 
it 

;  03 
•  >, 

:"c3 
:1 

*>£ 

K 

+i-^ 

j9 

+s  O 

BJ-d1" 

•rt 

-w-d 

— 

■ 

4^ 

■  M 

"3  = 
coC 

P 

mm 

3 

OQ 

-3'L 

GO 

03 

CCPh 

- 

p 

•  a; 
IfC 

:o 

■a 

£ 

£ 

p 

SS  :£ 

p 

& 

& 

o 

• 

0 

O 

•B 

- 

:£5 

A 

fl 

hI 

m 

00 

CQ 

02 

Hlfl        • 

:S 

•  co 

•  c 

•  io 

iO 

So1  : 

"H 

'.** 

1-1 

1-1        ! 

! '— ' 

I1-1 

lO 

oo 

e> 

■  io 

£ 

00    ■  0 

»lO          IT* 

■-  c 

'• 

s 

? 

S  : 

O  Tl 

O 

•  ■^1 

•<* 

-r  ^r 

O 

rt^ 

I1-1 

1-1 

"■'       I1-* 

IH  - 

rt  : 

_h  ,— 

r^C000-3<-tfi-*f<OOO<N 

N  ■*  rH  i-l  «5  00  rH  O)  N  «; 

mwiortoaffloot^irt 

csi  ooo m ic 

UJ^MNiC 

cn  oo 

iQLOio^'j'Mi-noartiosif; 

N»MiO«iiHH-HO0iOMt> 
OOOOO^tiOOtOiOiOiO-t 

•  e 

NNOOOC 

00 

OikT 

| 

O  00  CC 

:g 

-*i  O  O  10  t-  O 

toiOHoaoc 

r-liH 

i-H                                i-(  i-H 

1-1 

l-H  l-H 

MNNtOtOtD^HHOC 

O  il)  W  113  (O  (O  N  Ji  Lt  —  SO  —  IC 

•  a 

COMOOCO-ti*'J'OiO« 

oooo 

lOOOC 

Nr-lN^M000000HttO^ 

vioooooni^ooooiac 

1 1- 

ioo- 

T 

OOOCO'ViOiOOr-^O 

OJOSNa 

oo 

•  tti  iji  in 

oooco-^ioooeoo 

-1 

* 

rH 

oo 

o 

ONO 

OlOiOiONMNOiOO 

<o  00 

-  = 

8 

ooooomoooo^T 

C>)  IC  O  C")  ■*  N  tji  i-(                CO  CS 

:S 

■^OOiOOOOOi-HO 

t^  00  i- 

fMi-HCOt^CO        -*1  i-i  i- 

i-H  -q 

i-H  •<*  i-H  CO  CN  CO  CO  1 

8£ 

r? 

omo 

HiOOOOOOOujiON 
OOtN^Ot^cOiOt^O 
COCO^OOOOOOOi-HCC 

SS§8§ 

oo 

OOaiOlHN-^OJOlMMWT 

•  iCOC 

'NCOC 

mooootc 

-H  -O  C3  O  00  K 

8S 

OTT 

<X 

•  oooococot>-oo»- 

TH   1-1 

^rtrt                           ^_^H^H 

HriHrtr" 

i-Hi-H 

HHH          HHHH'1 

,-l,-l                   r- 

rH^ 

B 

*B 

&■* 

3 

dgepor 
uchan 
chanan 
av 

■g'S'Si 

a 

OS 

.-O  fa  ! 

■  oOej 

T3 

5 

rt  d-d  fe 

03  03  0  2 

x^ 

:s 

:^S 

c   .-d 

fto 

c 

o  o  o  & 

b 

•  ©  fteL 

O 

- 

1   • 

B  B  0  e< 

'  - 

■  ©  & 

•    O 

c 

c 

c 

C2~ 

H  to 

T:   -* 

&l 

T* 

J  6  o 

22  £& 

'S'S^'d  c 

&a  HI 

•  9- 

bi 

I'd 

3    . 

0   O 

afiaie 

0  03  rfl 

"H-b 

~ 
3 

"CW  B£ 
ffl     Mod 

.3  .fa  .3  •£  "d  "d  *d TJ  s O 

mwwfq  :  :  :  :m- 

SS 

S-. 
PC 

-d-d  d  g.Ht'O  S3O  .fe-B.B 

:   :pqpqWpq    loas  02WW 

iff 

-CTT 

?s 

'E'd'd  z 

pa  :  :pc 

O-B 

r~ 

,Jp 

oo 

T* 

■* 

CO 

«*             10             10 

— 

»o 

* 

-r1 

"* 

TJ1 

T>i              ■*               >tf 

' 

■^ 

6 

0 

O 

O 

0 

0 

•> 

„ 

03 

M 

§ 

ft 

ft 

a 

a 

a 

a 

1 

a 

a 

a 

a 

a 

03 

hi 

>i 

>> 

>. 

>> 

■s 

03 

c3 

03 

03 

03 

w 

w 

P 

P 

p 

0 

P 

a 

p, 

B 

B 

B 

B 

0 

03 

03 

03 

03 

tj- 

-d 

d 

a 

a 

3 

a 

05 

PQ 

OQ 

OQ 

00 

OQ 

S3 

414 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spjxeq— ipnpcud  I'Biijni 


^  2 

£2 


rt  03  O 
££2 


WPh 


•a  :5 
.203  :Ss 


ol 

8M  : 


CGPh       PQ       CQCQ 


00 


•199j— qidgp  ib^ox 


•188j— qjdap  no 


•J99J — 9TTBld 

ran^Bp  9AoqB  aptvmpy 


^NNNNtOOlOOOOOOfflO*  CO  t^  < 
'iOO)«0)«H(NHLOt^iOOINr(3N  t^  CO  < 
iNOOOKJiOiONOOiMOiCOOtO       iO       Oi 


10  lOOi 

oo  >o  CO 

ooo 


•^88J— I8A9I 

■Gas    Avopq    9pn;iip7 


•}99J— 

pa^BJigngd  ssanjpiqx 


CO         ■>*  « 
i  C$       i—l 


*199j— do;  o%  q;d9C[ 


OOOOiO(MOcOOOOOO!-iOiOOO<M< 

OOOlOiOCNCOCOCOt^OOrHCO^^I 


>>ls  >» 


°  2 

o  P< 


03    •  o  o  g 
Pi     •  o  o  P< 


03  5     > 


•doo 
'C'a'O 


3  o  ®  03  PI 

m.2  ©  >.2. 


w  :  :  loos  coWw 

:m^  MMpq 

:  :pq-  Wpq  is     W 

WM 

pq  :  : 

o 
eo 

o 

§ 

o            o        oo 

O                CN           <N 

o 

o 

6 

6 

6 

6 

fe 

B 

£ 

fc 

a 

a 

a 

03 

PI 

03 

s 

g 

s 

6 

a 

s 

fii 

,4 

a 

43 

co 

co 

CO 

CO 

Q 

H 

H 

H 

W 

Pi 

o    . 
23  o 


a 

— « 

t-t 

(H 

h 

fca 

0Q 

CQ 

02 

n 

pq 

PQ 

PQ 

T 

50 

r-i 

CN 

T 

BLATCHLEY] 


TABLES    OF    WELL   DATA. 


415 


a 

c 

S 

or 

- 

% 

.    •  « 

PI 

; 
! 

! 

s 

r 

5- 

1 
s 

CO 
"c3 

>- 

II 

03  — 

a 
C 

c 

"z 
a 

<2   . 
o   ; 

o^  ; 

j-Ti-i 

05   CO 
"cits 

'3'cl 

mrn 

co 

BO 

§ 
■a" 

0 

fH  — 

-  i 

cc 

§ 
oc 

c 

<3  So- 

a«ji 

52^ 

CD 

3 
"c3 

"c3 

CO 

-J 
CD 
<D 

5 

O 

3 
'S 

« 

DQ 

CM 

OS 

a 
i> 

s 

« 

53 

5  5  : 

•s  : 
cq  : 

OOt-H 

COO 

CM 

O 

to      o 

o 

00 
CO 

CX) 

TPCOCO 

CN 
OS 

5 

||  :| 

3 
3 

CO 
MO 

ooo 

00 
8 

2    8 

eo      co 

o  c  co 

CO  CO  CO 

00  :  i 

iflONLOo^    oo    ooi-hco      oooiocoMinooo      tooooioteooom      3OLO10 
o  t—  co  o  o  o    o    oot>co      o  i— <  o  o  o  00 1>- co      ioohoooioooom^      io»ococo 


»1'S)M»50>201iaOL'3 


iOO»COO  CN  CN  O  t~ 
lOOiOf  N*  CM  i—  'XD  -=n 
VOOOO^'r^     <J<    cot^oo 


t  N  lt  f»  1>  10  CN 
CM  00  CO  O  t~-  CN  O  ' 

■>a<  co  •>*  »c  10  co  t^-  ' 


oo-^co,»,^riccocot^i>- 


■«*"rT)<■q<co'^ooco•,*'*■^,■ 


O      lO  CO  CO         f  Mt-OMMOM         OlNWlflJOOM 
CM     lO  i-H  CO        CN  CO  lO  CO  i-l  »C  CN  CO        NHHN^iOH 


OOirj  lO  00       NON 


lOWOOO      •  m  lO  CN 


:S2S 


HON     •  >o 
n-HCO      -CM 


iO  ©  00  lfl  CN  00 

Cs  -r  02  00  10  r~ 
00  CM  CM  00  00  00 


Of^iO        NiOOOOOOOiON        ONOOiONOOOO        OOhh  00 

lO  CN  00        CO  >— ico-ri- iiOMffi        Ot^NiOOOCOCfflN        -<3<  O  O  CN  CO 

O  <M  (M         00  00  00  O  O  O  1-1  CN         MOOOOOOOOCSOHHrt         COCOCNCO  00 


00  CN  O  CO  lO  O  1 


1  ©>o  O  "CO 
110  -«  r-  00  ~* 

000  00  000 


■  o  P< 

>  ® 

5  .is  •£  "0 13 
Mpq  :  : 


d      .  o 
OSS     fe 
O     *§  03-^ 
•O     30-3 

:  «s  M 


■O  O  O  O  O'cj  flr* 

"C'3'3,3'3  d  j3-a 

pq  :  :  :  :pqa5W 


•    OJJ J2    >>     • 

OT)  OOOO  O  o  C3  O 

*3'ni3,3,3,3'3  s^j'c 
;  ;  :wco  : 


5 


o  2 

o  P< 
.    .    .    .  K  M   .    .    .    . 

OOOO'g.'C'OOOO 


:«w  : 


0 
■*J1 

O     CN 

-V     CO 

1J1       TJ1 

00 

CO 

00 

CO 

CO 
CO 

CO  00 
CO  CM 

0 

COCO 

CO 

•»J» 

0 

10 

10 

m    in 

TJ1        -^< 

t~-  .      CO     CM 


z 

fc  z 

z 

z 

fe 

zz 

a 

c    c 

c 

S3 

S  c 

a 

C3      C3 

C3 

03 

C3 

C3  c4 

i 

s  a 

S 

s 

g 

ss 

CO      <» 

0 

CD 

CO   CO 

- 

^3    A 

^ 

fl 

^5 

^£ 

eo 

co     co 

CO 

CO    CO 

w 

w  w 

w 

s 

w 

WW 

o  o 


000 
55  ^  Z 


—     —   — 


pqpQ 


o  2    2    2 

2  2  2  2 

O  OOP 

°o  0s   S   si 


416 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


1 

© 
to 

o 


•sjgjjeq — ^onpojd  i^iui 


•}88j— q;dop  ib^o  j, 


•}99j— T^depno 


•;8aj— Qwe\d 
xnn^p  9Aoqe  apnji^v 


•;)99;— J9A9] 


•}99J— 

p^BJigugd  ssgujiorqj, 


•;99j— do;  05  q^dga 


9* 


iHioocoococoiCNoO'^t^oiooioootooin-o'iO'*'*      (ocoNtotom 

>OOO«3OOOOOc0OOOO05C0>-tOi-H05i-ii-iO        rH  i-H  ©  CN  ^H  Oi 


^  TP  rji  ^t  CO  ^  ' 


WOlOHOlOOINOJOON*      .(N-*©      •©©      •  lO 

CN  .-I  IC  lO  NHHtOHTfOO        •  1-<  CO        •  i-l  1-H        '.-H 


«5t^OOiOiCNO-*iNLOO)OOOOCOTt<iI5lN(NOOOrtOHH        NNlfiOOH 
gOiOOOOgPJNWMONOt/jNOOlOO^OOHCOM        OmOH^OO 

ooo2ooo5<Nooa>ooo50icoc50>ooo>oc>)ooo50oo>c»ooo5      oo  oo  ©  i^  oo  © 


°  s 

o  Ph 
P  Si 


O  & 


bo  .    .    !  ?  m  !    .    .    ;  P  be  !    '.    '.    !  >A  &c  '.    '. 

too  e^J  o  o  o  o«2  °  o  °  0,rS  o  e  o  o  o  o      ooo 

m  :  :  :Un  :  :  :  :Mw  :  :  :  :Mm  ::::::     :  :  : 


=  o  ©  <s  a  © 
cn^»  >.2.2 


co    ior-      co      CO    oo      iO 


TP       W 


c 

£ 

tN 

CC 

oc 

? 

c 

s 

oc 

■^ 

i^ 

« 

CO 

B    B  5?  5? 


ooo 

B  ££ 


ooo 
B   B     55 


03  C3C3C3  03  CC       C3    C3  C3  03       03  q 

o    6  o  o    o    o  oo    o    o  6    PQ 


SB 


■rj  O 
03 


c3  ^03  (C6  #w 


o 
o 

3 
O 

O 

3 

c 

o 

3 

0 

o 

O 

o 

c 

O  O 

33 
oo 

c 

1 
9 

o 

3 

9 

c 

3 

3 

QQ 

CI 

8 

3 

3 

8 

88 

h 

co 

co 

CO 

N 

CO 

BLATCHLET] 


TABLES    OF    WELL    DATA. 


417 


0 

- 

r 

CN 

s 

a 

t 

— 
a 
EC 

8 

CD 
,g 

IO 

Bs 

~~ 

— 

3 

X 
C/j 

© 

ft 

A! 

§ 

CO 

-d 

ft 
US 

© 

<£ 

N 
X 

OS 

c 
o 

CO 
09 

fl 

cc3  a 

n  — 

Woe 

CO 

so 

0 

— 
a 

E 
- 

T 
- 

r 

!  © 

■© 

■iO 

© 

§ 

-d 
© 

- 

Is 

« 
H2 

d 
fl 

'3 

G? 

"©  ; 
©  . 

8  : 
o  : 

1- 

co 
03 

o 

e 

3 

« 

O  > 

1 

s 

CO 

Si 

M 

Oi 

o 

o> 

i  - 

CO 

iO 
CO 

C5C5 

oo 
co 

C5 

s 

oa 

5 

ooo 

OO  CN 
00OC3 

1 

CO 

t-JO      -00 

00O       '  OS 

O  IO 
!>■  CO 
t-00 

©■SCO 
00  CN  -1* 
CNCOf- 

omooo 

00  00  OS  00 

o 

CO 

—  t^iot^r^t^cocoic 


00  i-H  CO  iO  OJ  -^  C5  Oi  i-H  C5  C5  O  —  X  CO  'O  3>  «C  M  X  3>e0CNC0C0rHC0e0t~O0iC0t~O«0O00C0a»< 

HlOO'<iiNNN'WOO-?ONO»CSiHH^KX'NCM)CNTCDONl,OOffliON(>J( 
ujHrtCOOOOOOOtOhffliCHOCOOXCCOulHOOOOC^NHOHHOHHM 


N   ~   -  Ll  H  L-  , 


IhOOCN^i- 


t  t-  oo  co  eo  -v 


i  r~  cn  i-i  r~  oo  i 

inomcoocooococo-hni 
jooojco-vott-^coooook 


■  *oi'fl"i'KCH-?KoinoNT(iHO 

iCO-WCOOCOOCNCOTCOCO-fCOCOC^OO 


r~    •  o  io  io    •  io  c  cn      l-c^-l-^onvo- 

■V      'COi-HCO      •  l>.  TJ>  CO        ^-CCC^r-^^liO^-lCNCOCO' 


I  . — I        NrrrHt^I>  COi-1        CNt^iO        CN  ,-H  O}  CO  C^  CN      •  rH  CO        CO 


rtCtfOLloOOWOOBNaoONHiflOCSiOffliOOiOOOoeMaiOOOOMiONH 
MC-.K^rNNOVlOOMHMNNKMM  C  ~  i  -  CO  ::  I-  CO  MC  A  Ti  —  M  rOOONO^O 
—  f  -  nr  r*l  nr  —  c^  ,— n  ,— s  —  **^  ^i  r\-s  /^\  i —  iv  *  *  —  <-^  ^]  ^  ^  •-•  rN.  r/^  ^  -^  ^]  ,-r  r  -  nfi  m  ry  rv"  r~  nri  nr*  (M  /vs 


jgOOOl 
4  §  00  88  o»  i 


r-  x  X/.j.M 


-^  *— ;  I'-  1—1  "J  *~-> 
lOOCONMCCNKOOO^ 


COCONCOC1C    X    ri-MOOUJONlOTI 
CO-^t^00O5i-KMCOt^00O20000O50000CN< 


d  c3 

-co 

pqs 


o  ft 

^T)  OOO 
•3  '£  dd  d 

M«  :  :  : 


fld 

C3  O 

12 


c 

©  60 

«d  o  o 
S'Cdd 


■rHCN      " 

•'-d-d 


■  g-d 
1  o    -Soft 


So 


■rHCN  •       • 

i'd'd  I  ^ 

■  o  o  •  © 

•  °  o  •  ft 


C3      •   O   ^ 


O  O  O  O  O"o^ 

-c-dddd  s-^0---«'C'dd'd'd  so-- -A  2'Cd-d  so  . , 


k  ?  m   !    !    !    !  2  "J/i  >*  *  ©  to   .    .2~/i^60.    .    . 

•tcC'dd'd'd  SO---3  2'Cdd  sO-A'S'd'd'C 

:cq-  ^^EHw  :  :pqs  ^^  :  :  : 


O  O  O  O  03^ 

-d-dddo-fl 
!    !    !    !^  M 


^    !5 


tf       « 


0 

0 

0 

0 

— 

» 

» 

!? 

^ 

- 

u 

© 

^ 

* 

■5 

& 

* 

0 

0 

0 

0 

0 

w 

CQ 

pq 

pq 

- 

■d 

d 

-d 

-d 

d 

d 

C3 

c3 

c3 

ao 

a 

co 

co 

CO 

© 

© 

© 

© 

© 

is 

^ 

* 

^ 

* 

0 

O 

O 

0 

0 

PQ 

pq 

W 

pq 

CP 

t^.  00 


.2     -2 
5      d 

■*      iO 


I  'I 

co     O 


—2:  G 


418 


OIL  FIELDS  OF  CRAWFOED  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


sjajxeq— lonpoid  ibijiui 


•ijaaj— mdap  i^o  j, 


•jaaj— x^dap  no 


•^aaj— atreid 
ranjtjp  aAoqe  apn^iv 


•188J-  T8A9I 

■eat    Avojaq   eptvmiv 


laaj— 
pa^j^auad  ssaujpTqj, 


•;aaj— doi  oj  itfdaa 


3oi  cfe  fl' 


S* 


§  . 

•43  O 


s& 


c£ 


£dn 

00  O  ® 

•,T3   S3 

<3S« 

s®  2. 

-t^!-'  ,;o 


I  LO  lO  t-  - 
)  00  03  t~-  ( 


338 
COOOO 


a»ooio«ocococoooioos      "5  < 
■*  gj  »o  oj  o  co  Tti  as  a>  oo      oo< 

HOlHONOtOHOlffl        CO  < 


)f-05C0C0C0 

'tOHOMO 


fH  2J  io  io -^i  tj<  r^  2J  io  i-i      ioNN'*HoaooN«HcoaicoMOONNH'* 

lOO^NOHOOOOH         HNCOOOOONHNiOiOOlCOffltDCOCDmOtOOM 
0010CO-3<<N''fOOCOlOOO         0000CO"^,CO"^CO00CO'<fcNCOCO'fCOI>'00C0  ■f  r-  CO 


MTfOOOONNiOtO 


l^  CN  10  CO  ONOMwONMiOfflOOO-^OOOMNMMOM 
rtffltDiO  ©MNNNOHNlOiOt-NtOiOMtON-JiOON 
COC^OiCN        CN  CO  00  Oi  00  OJ  00  CO  00  03  t>.  00  00  Oi  00  CN  CO  00  O  CO  00 


•d  o 
'G'd 
PQ   : 


>  a. 
O  O  O  O-jf  d  o 

:  :  :  :W«  £ 


°  s 


O  ft 


o^oooo«t3ooooo 

:Wm  :  :  :  :mpq  :  :  :  :  : 


O  C3 


o  ft 

£d  o 
.h'Cd 

Mm  : 


s 

Ifl 

CO 

© 

o 

10 

?! 

0 

c^ 

t" 

10 

!«• 

_, 

OS 

eg 

-T 

CT> 

S 

■"* 

Tf< 

•fl 

"* 

"* 

■* 

-r 

•v 

lj 

tp 

Tfl 

© 

t*. 

OS 

cN 

»H 

tH 

OS 

CO 

1—1 

>"< 

•-1 

"H 

•""• 

CN 

O 

o 

o 

o 

o 

O 

0 

O 

0 

O 

O 

O 

O 

0 

O 

O 

£ 

B 

£ 

ft 

52; 

ft 

1? 

ft 

fc 

ft 

fe 

* 

ft 

fe 

2 

55 

eg 

.s 

BO 

OT 

sg 

CO 

CO 

g 

a 

eg 

.2 

ryj 

X 

CO 

a 

.a 

1 

is 

* 

Is 

* 

fs 

* 

* 

* 

* 

£ 

is 

* 

% 

fc 

i 

J 

-3 

■J 

0) 

^ 

3 

CD 

3 

CD 

3 

3 

■3 

j 

J 

3 

^ 

.2  .2  °  2  2  .2 
2  2  2  2  2  2 
o    o    0000 


2  °  2  .2  2  .2  .2 
2  2  2  2  2  2  2 
0000000 


§  s 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


419 


O! 

0 

a 

« 

a 

C 

Saltwater,873  feet.    Well 
abandoned 

Gas,  l,270feet.    Red  rock, 
1.220  feet 

•  ■4-3 

is 

-ClOS 

•P 

Si 

£  : 

-U   O 

73-d 

1 

a 

P 
3? 

IS 

s 

i 

BO 

5 
M 
d 

ss 

o 

3 
o 

43 
02 

1 

8 

CM 

£2 

0,-h 

43 

GQ 

o 
55 

U3 

■*CN 

lOlO  to 

1 

00 

s 

o 

S 

OS 

IO  cm 

oo 

SO 

S3 

<* 

90 

U3 

OS'* 
t>  CO 

wo 

ioooco 
lO  io  »o 

2 

s 

- 

- 

CN 

r.  /- 

o:  X 

s 

| 

o  o 
1-  ~ 

CO  -r 

s 

«5tOU5C 

coco^-r 

a 

ou: 

ior~  oo 

(NrHCN 

S8 

oo  >o 

io  co  t-  to  co  o-  oo      oo 

iji  Tfi  OS  O  ■*  OS  CO        CN 
JO  i-H  OS  t^  CO  »H  1-4  O- 


OCaCONINNONCOO  OOOOJOJfl'NCOMNt^NINHfqoONh.OOOOlOOi 
iHOOOiOOON^^CftM  C»TPt-fflCOO>O^NMtlONOlO«)NHOOHONOOlfl< 
HO!OC<10)00®iO'*N        00t0iOON(0ffllOt»(00SMN!0iO»0l0U3lO(D'*01iO' 


00  CO  IO  t-  00  CO  CO 


HHNOOOOMOM' 
00i-IOS'Tfi-lt^<O»O< 
COiO-tfiCNiOCOOOCSC 


IHHtOCOCO' 

1  CO  COOOS  tO  t  .  - 

>  Tf  o.  oo  oo  os  oo  c 


)Oioosoooeoco< 


NWOOOH- 


2  8  333  to00  8  23    8! 

i-l  CN        i-l 


iSSSc 


lOOOONOOOlMOOOO' 


CO  00  O  CO  CO  00  oo 


ifli<5NOOU3(NO 
OO^HOOiOtNt^cOCO 
OOOOSNOrtCO'fl'lON 


O        OOOOOiOKJINi 

CO        O  IO  CM  CM  CM  OS  00  -#  < 

.-I  CO  ^  OS  CN  CM  CO -<J<  < 


i^^iiO^iOi 


■  O  "O  »•  C~  <N  -*  CN 

>  CO  CM  rH  O  IO  l>-  CN 

i^ifliOWMMiO 


-d  b 
o  2 

o  Ph 


^■d  O  e3^' 

•^"do-P-- 
'sMl 


Mm 


'd  o  o 
Cd-d 

n  :  : 


p„ 


-d-d  so 


d'd  b  ii  i 
°  °  2  2 


O  O  03 

£8,5 


^^C'CWo^C  P£sO;S3£OCd  p 


o-~ 


So 

|#a 

£CO 
Mm? 


•goo 


3  8    § 

10    IO      10 


1*1  o 
O  OS 
IO    ^ 


8     CM 

•O     IO 


IO       Tt<       IO 


CN  "•'  O 

CN  .  CN 

0  d  d  d  «-' 

55  !?  %  5?  d 

www  g  <^< 

£  '£  '^  'fe  "3 

co  o>  ©  a>  cp 

^  J  J  J  55 


o    o 

5z;  £ 


fc  5z; 


"cri    to 

t^ 

IQ 

■re 

00  <N 

— 1 

O     O 

0 

.-. 

O 

O  O 

0 

fc    » 

% 

^ 

Z 

££ 

z 

43    -=3 

A 

43 

43 

43  43 

43 

60     60 

01 

sr. 

(=r. 

tUDbfl 

ES 

P      P 

P 

p 

P  P 

5 

C3      C3 

BJ 

03 

C! 

c3  c3 

OS 

•d  -d 

■d 

T- 

■d 

-d'd 

■d 

-d  -d 

T3 

-d 

-d 

."SS 

d 

s  a   sss^   s 


c3         ^     ^  9 


5  S 


00000 


4= 

43 

43 

43 

,2 

£i 

43 

A 

43 

43 

43 

-3 

^3 

43  43 

43 

0 

O 

O 

0 

02 

CO 

CQ 

02 

02 

02 

02 

02 

O 

O 

2 

O 

O 

OO 

O 

OS 

q 

rH 

S3 

^H 

CN 

* 

CO 

l> 

00 

OS 

O 

— 

CN 

CO 

TJIIO 

CO 

420 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,   [bull.  no.  22 


•spxreq— lonpojd  vsmni 


•^98j— mdap  \e%oa 


•%&&}— i^dep  uo 


nin^p  eAoqc  spnipjy 


138S   ^ojeq    epn^T^v 


188J— 

paiejianad  ssaujprqj, 


•^98j— den  o;  mdaci 


6  Si  c3  fl- 


1 

<->   gj 

§JH» 


.00 


o  o 

CQCQ 


3K  :£§    83 

0000     •  00  00       CT><3> 


:8 

IS 

CO  o 

•g  ass 

i  ii 
•9  gg 

5,  'S'eS 
C7   COCO 


'NOOCOOONMMN        C5  t~  O        CM  t^  t>.  lO  t 


'ONtOOH  oo< 


CM     CO     HOOh'*© 

i  cq    t^    cq  co  t-i  Tp  t^  »-i 


O  CD  00 
■-I00CO 


CM  Tt<  CM  CO  t-  t~- 


00       lOcO' 


00C0C0»0O        OOiOOO     rt<     OiOOCOcO" 
Ci  CO  Oi  00  CO         00ON      CM      t^-  t-  O  m  <N  C 

co-^Tjico^      ^*ioeo    tj<    co  Tt<  c^  oo  rt<  • 


■»OtDiONOHiOU5I 

CD^^H00CNCOt>.O5lOC_ 

00  CT>  CM  CM  OJ  00  00  00  O  Ci        CNOOOO 


00U5O     CO 


OOMNW 
-  .  CM  -*  O  t-  CO 
00     00O3CNCO00O5 


T)  O 

pa  : 


CS-^'OOOOOO        ced  o 

2  Wco  :  :  :  :  :    s  pq  ' 


o  o    . 

O  O4    • 

S^T3  O 

Wpo  : 


3    S  S     5 


CO 

Tf 

<N 

CM 

*H 

o    o 

Jz;  fc 


0 

0 

6 

6 

ci 

6 

!4 

fc 

fe 

£ 

fc« 

» 

t-> 

tT 

"O 

■d" 

-o 

>» 

>> 

>> 

t*> 

0 

0 

0 

0 

S 

a 

n 

pq 

PQ 

PQ 

c 

a 

0 

0 

0 

0 

ft 

Pi 

ft 

ft 

ft 

ft 

<Tp 

& 

a 

M 

60 

bo 

W> 

Xi 

•s 

T3 

T3 

>d 

-S 

PQ 

PQ 

PQ 

PQ 

PQ 

PQ 

ft  • 

as 

a 

o    . 
"3  o 

s* 


1* 


B  LATCH  LEY] 


TABLES    OF   WELL   DATA. 


421 


03  03 


d 

wig 
•IS 


+f  co  d 
r3  o3  © 


I  :"3 


3 -2 .2 -a 

O  »-*  co  t> 
£os  o3  P 

m    o 


il 

.  0  . 

•CO      ' 

:i 

ilH      ■ 

■  +3 

•*3      • 

•S  : 

•QQ 

•  o    . 

■  « 

+£*■*    '. 

;»o 

£M    '• 

=>  o    . 

O     (H   +J 

'   OS 

■H    CD^H 

:o 

rt 

iflO 
i— I  OS 
<0  l« 


■aa-a 

3    *q 


oioio 


©  OS  t^  O  00  r-«  CN  CO  I 

00        CO  ^  CN -«f  CO  .-(  CO  < 

1-H  OOO— l©T-<OOSOS©0< 


OlOHOU5CNlMC»l010NNCONN         ^H         t^  CM         .-H         <M  l^ -<Ji 

O^rHCOHOCO'O'HCOfflNlOt^^         O         f  00         CO         CCHN 
NrtHOOINHOOWN^OHH  C  ©OS  CO  ^  ■*  r-i 


'  CO  TJi  CO  ■*  IC  *C  ' 


lO  •>»<  Tfi  lO  CO  CO     ^     CN ->3< 


O  iO  OS  O  lC  00  00  i-H  lO  U5  CO  CO  t~-  CO  00  OS  CO  < 
©  -f  00  Tti  00  OS  CO  "*  00  CO  O  l>  -*  CM  lO  OS  U)i 
CO  CO  CO  ■>*  -v  CS  CO  •«*  >*  CO  1>  t-  00  CO  CO       ■"*       ■*> 


oo     ooco 


iNO>g 

ii-teccN 


llOHM»H0010lOOOtOOOO  »o  w< 
iCN-^OOcO^NCNUDHioOOrti  00  iOi 
I0300000SO00  OS  OS  OS  OS  O  00  00    00    r^< 


WOV"20m>0»NNOOTPiOO 
(OHWOiOtOMOiOOt^VHHiO 

t>ooooosost^eoosos»-Hi-icNcooooo 


03  O 

o  & 


lOoooo'SDoooo'S'do    o    oo 
I'S'd'S'd'd  s'jj'd'd'O'd  s'S"^  ^  d  t3 

:  :  :  :  :  :pqpq  :  :  :  :pqpq  :    :    :  : 


o  o< 

>»   CD 
OOOOOOOOOt3o303^'dO 

::::::::  ima^  W«  : 


p»5 

8°  bo 


B§fQ 


CN  o    coc 

t-  CO     co  CO 


oc 

K 

t> 

IC 

Pi 

D 

C 
1-1 

•*  o 


o 

o 

O 

O     o  ^ 

o 

fc 

fe 

fc 

fc 

CD 

03 

03 

-3 

"ca  'cs'ea 

"3 

pq 

ft 

pq 

pq  pqpq 

pq 

3    53 

O 

o 

3 

ft 

ft 

Ph 

CD 

CD 

a 

bfi    bCbxj 

bfl 

bo 

T3 

•d 

•d 

(H 

pq  pqp 

pq 

pq 

pq 

422 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,     [bull.  no.  22 


•sisxTBq— }onpojd  tbt^tui 


•;98j— itfdep  ib^oj, 


•%&}— q^dgp  \]Q 


>woo> 


IS 


©5 

02  Ph 


r^co 

CO'*' 
COCO 


<x> 

3 

.£ 

a 

o 

i 

eo 

S 

© 
Eh 


•^93J— 9UBjd 

ran;Bp  9AoqB  ©pn^i^v 


co  r~-  co  co  »o  i-~  co  ■*!  o  i-^  Oi  co  oo  co  i-H  co      TfcooioO(NN'<ji(N^mcqNO! 

OffliO  OCOIOOOOCO  O  OO  OO  O        i-HO  ©OO  .-H  O  COi-H  Oi-H  OcO  o 


•^88J— 19A9I 
B9S   ^ojgq   optupiv 


i(DOtOHHHTtlt»HHMlO 

lOiiOOir^t^iot^Tticor^t^o 

'  00  05  tp  00  OS  -en  r«<  -tfi  00  T  Tfi  -^i  rf  Tji  tji        CO  TP  f  tj<  rt«  CO  •*  00  C0  f  CO  ■*  00  OJ 


•J99J- 

p9^j^9U9d  ssgu^oiqj, 


NTfHNHNi 


:j99j— do;  o*  q;d9Q 


hoom^ooooowooNoo 
1  ©  co  co  ©  ©  ©  cM  oo  ©  oo  ©  ©  oo      oo  ©  ©  ©  ©  oo  ©  cn  oo  oo  oo  ©  co  eo 


-    C 
.     PhO 


S  2 

o  a 


8  a 
,  .£$  . 

o  o  o  o  o  o  o-M*d  o  o 


g-C,d'd.a-E'd,d,«rd'd     "O  t3  -d  d  -d  d  *  .a  'g  -d  •© 

hpq  :  :Mpq  :  :  :  :  :     ::::::  :Mm  :  : 


o£o 

-d-a* 

:M  : 


B 
03 

C5 

2 

£ 

A  a 

o 

>  o 

<2 

•^ 

;s§  s 


o  o  o 


M       MMM       M       M 


o    ooo    o    o 


o 
to 

OS  O 


CO 


o 

3 

O 

O 

'-alaia 
OOO 

o 

,3 

o 

O 

A 
O 

w 

•— 

e 

CD 

8" 

cNcoeo 

CM 

CO 

CO 
CO 

eo 

CO 

<N 

eo 

■v 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


423 


22 

03   03 

■a'a  - 


- 

i 

i!- 

So 


"3  = 

d  - 

c3  00 


pqW 


n 


e*S 


.o  © 

■©  s 


83 


I-3 

£  09 


•_-  = 


2Sc3 


>*»OOON 

re  co  x.  oa  re  re 


re  re 


8l-  s  o  l-  x  ri  c  n  c  m  c  a  «      mohon 
oSoaot«ioco<-io<o<o<o>oa      co  «o  »-•  as  so 


X  a  re  iC  93 


>aa>Oi-ii-iH      nfirrcxbHKcaaNxc 


iOHO)oa 


:  r-  i-e  ac  ue  -h  c  c  c 

sNKNNr-Hrjc-CMZ^       r:  ~  i--  -  — 
I«Ohh»o£XC:  re  re  re  re  C;       re" 


i-i      eo  re  -^  -^  i-e  «  o      coooaoo>ococo>oao<3>0<HC^ooco-<3<>o>oeo^^< 


In 


=i1 

log  . 

.a  o-r  "0 

ag«  : 


«■ 


WMeSS 


©  © 


- 

bi 

•_ 

Sh 

d 

— 

G 

— 

d 

pq 

3 

w 

pq 

CQ 

33 

02 

CO 

CO 

30 

rs 

O 

•"• 

CM 

re 

424 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•siajaBq— lonpoad  p^rai 


laaj— qidap  iejoj, 


02 


iO  en 

co  <S 

O 


•jeoj— q^dap  no 


•laaj— etrejd 
ran;Bp  8Aoqe  opnji^v 


0)<NmOONMNOS(00>OOOOHCOtO«5HtOrtlOt00300c5MOO©C«5 
■*MNrH00(N(OlO0)rt00Ht0^OOrtl^N10t0H«lOtO!D'«<00H 
lOiOO'ft'VCOiOiCMCO'OiOOOOOCiMC'ftOfflOtOMOiOCOM 


•J88J— 18A8J 

eas    Aiojaq    aprnx^v 


^OMOO^t^CO^OOO^OOcOCNlOSOSCOc^C^^COOOt^OCOCOlOi^OO 
0)050iOJOOOO)0)HH0500'*«)0000»HOOOOOOO*05'H0005'HH 


•}aaj— 

po^j^auad  ssaajpiqj. 


•  "O  CO  1-H  OS  "Cf  CO  "O  <M  CO  O-  <M  CO  CN  00  t—  t-  CO  00  CN      iCiSNtOUJOO)      •  f 
I  CN  T-l  <N  CN  .-I  -^  i-H  ^H  -<TI  ■*!  r-H  ^  CO  CO  "0  !-<       <  CO  ■*  •*  i-t  ^H  CN       ■  i-t 


•J99j— doj  o;  q?daa 


iMt^iOOMMaw 


-'T'COCOIOCOCOOS'<J1C©CO' 


o    •  o  o    •  o 
o    •  o  o    •  o 


M 


>>  :  :  I'go'g^ 


££ 


02 -2  «  >.2«2 


r  sm 

^Mfe 

*rw 

:SS 

3W  :pq"M  :  :s~ £s  WmMS::  V 

45S 

co 

CO 

OS 

CO 

CO'*!          i-H          i-l      CO          CO          CO      00      <N      t- 

COOS           —1           l-Hl-l           ^H           _|       r-l       »-(      O 

^rp        O        iCiO        >0        10     10*0*0 

OS 

M        H     N 


O         O  O 
2        22 


2  2     ^     2^2 


o      o 
2     2 


be    be    be   be  be   be   be  Mi   be   be  be  be 

.a    .s    .s  .g.a   .s  .s  a   a   a  a  s 

03  c3  ^        ^  ^        ^        ^     <rf        ^        c3o3<^ 


.a  .a 


a  a 


§  . 

"3  o 
"2 

GO 


4 

fl 

A 

AA 

A 

fl 

— 

A 

A 

A 

^ 

fl 

^ 

o 

o 

O 

OO 

0 

o 

o 

O 

O 

O 

o 

o 

o 

TT> 

r-i 

CM 

CO 

■^i  lO 

CO 

1 - 

oo 

OS 

o 

— I 

w 

ro 

TT 

J,  * 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


425 


— 

■2 

— 
r 

— 

5 

i 

- 

-7 

>~ 

I 

-c 

5 

K 

| 

$. 

a. 

<~ 

•4- 

0 

a 

«2 

s 

I© 

a 

0 

1 

o 
03 

1 

P 

o 

-** 

93 
0Q 

1 

© 

o 

+» 
t> 
os 
25 

s 
& 

GO 

1 

'3 

- 

8 

C 
t 

r 

K 

1 

•- 
a 

r 
— 

a 

i 
§ 

o 

s 

3 

8 

1 

1 

o 

O 

i-O 

o 
>o 
CI 

i_3 

— 

co 

CO 

8 

.    00 

so 

co 

I- 

SB 

OS 

CO 

cm 

^ 

OS 

o 

■q*  lO  CO  lO        CO  ■"*! 

ooseq 

(OtON 

CM 

-3 

OS  OS 

©  lO  »0  -f  CO  -"J1 


COCOiOCMCMCMOSOOOSCS- 


>WMNOU5lO( 


CDOOirHINNI 


r~  t--    oo    Noiot-oiojceiiO'j'ooifflnHinNCNMoooooNnNcooo 

i  -CM  -<f      CM      iQMWCjNHOOOOOiOHHHOHOOOONrtOOHrtON 


13885: 


-*i  -sf  OS  00     CO     tOt^NiOKOOOOr- t  CM  i— li— I  CO  -f  rfi  C^  l-~  00  < 

HOINN     r-l     t-OfflNOHHiOMiOCOOOtO«TliCq( 

aosOH    cm    C5  fh  i-H  th  cn  co  rti  •<!»<  tp  tjiio  os  eo  eo  eo  •^  co  ' 


lOiOHa-aiOHOioooOM 

itOH»0)aiMONtD»CT! 

nooooocico-^rrcoco'^t-. 


TfNlOOMrov 
lO  CO  CO  O  00  CO  CO 
00  CO  *tfi  CO  CO  -f  TT 


'S38S 


QO00      ^H      rH 


OSMIN'OONiOlO 


r-i  CM  CM  CM  ON  ^H  ,-H   .  m  ,-(  ,-1  CM  i-l  CM  tp  tji  CM   CO^COi-ni-i   'CM 


OS  TT  if  lO  lO  TT 


OS  CM  CO 

t^-  CO  OS  w  v. 

CO     flOCOUICOOOOSOSOSOSO 


CO  Tf  ooosos< 


Ol  O  N  (N  o  W  00 
CO  OS  OS  00  OS  OS  OS 


tf 

oc 

CO 

t>> 

>» 

M 

44 

co 

ft 

ft 

A 

A 

* 

£ 

o   o   o 

fc   £   fc 


a    a 


i-H      CM 


o 

5 

o 

Pi 

a, 

ft 

CD 

<D 

© 

bO 

W) 

60 

TS 

•8 

-o 

Ph   0*   P4 


426 


OIL  FIELDS  OF  CKAWFOKD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sjaxiBq— lonpojd  psprai 


•:}88j— q^dap  i^oi 


•:}88j— q^dep  no 


a 
o 

o 

I 

eo 
S 

© 


•188;— etre^d 
taniBp  eAoqB  epiniiiv 


•!}98J— I8A9] 

■ess   AU)j8q   spnii^v 


•188J— 

psiBJiausd  ssaujioiqj, 


•^88j— do^  <n  qidsa 


3  8- 


to  .2  «  ^.2. 


sz 


a 

o    . 
S3  o 

©^ 


Ih   O 


ON®iOiCO<C(ONO 


>r^oocici-«*u-»ooi^oo 


|  oo  ic    •  t^ 


O     .  o 

D<    •  O 
®~    te 

#a| 

"CO-- 
Ms  M 


c 
o 

&i#a|a| 

coE-ipOs  M;  W 


■       -NHOtlMH 

CO  <N  .-I  CT>  <©  O 


sss 


OtDNMOOl 
■*  00  00  <N  CO  *C  ( 


:S  W 


lOOWf  OOOiOOO 
(MOOOOiHOOOOO 

ococoooosoco-tfi 


O  o  o  ° 


o  o 
d  o  o 


•E.b.fcrE-d  §.a.a 
pqWMw   :pqWW 


8S 

05  05 


iO*J<MOiOONiOOIN 
Tfl         CN  lO  CO  ■**"  TT  T)<  OS  rH  CO 


1<(OCOIOOOOMNOIN 

oo«mH5co$owo 
Tt<ooo50500050iOi-ico'v 


°  2 

o  ft 


WpQ 


3   C§ 

:  :pq 


g  :| 


8 


lO  lO        lO 


M 

oc 

C 

cs 

i- 

tx 

o 

o    o  o 

o 

o 

o  o 

o 

£ 

fc  ££ 

fe 

fe 

££ 

ft 

d 

end 

a 

a 

d  d 

p 

o    o  o 

o 

o  o 

CD 

©    ©  © 

© 

© 

©  © 

- 

O     .CO 

-Q 

fl 

£2,0 

,c 

a 

a  aa 

a 

a 

aa 

d 

s 

©  ©  © 

© 

© 

©  © 

Ch 

Ph   -- 

Ph 

Ph 

PhPh 

Ph 

a  aa 


OO 

aa 
©  © 


Ph 

Ph 

Ph   PhPh 

Ph 

Ph 

PhPh 

P4 

ffl 

o 

■"' 

<N     CO-* 

U5 

to 

t^  oo 

o> 

S 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


427 


e 
— 
a 

* 

EG 
* 

— 
r 
DO 

_y  = 

J? 

- 
c 
«e 

l 

- 

* 

1 

a 

11 

©J 

B 

— — 

3  - 

CD  00 

3 

B 

s 

0 

X  C 

"t  71 

so 

—  — 

P  - 

-- 
3« 

X  — 

— 

1 

f 

R 

3 
-_- 

i 

- 

I 

— 

■  X 

;a» 

:  0 

:S 
.« 

.  i-d 

.  i| 

j|3 

in 

- 

( 

r 
X 

— 

3 

0 

0  .    , 
so    . 

CO      .      . 

-o   ;   : 

1  :  ': 
io  ;  . 

1  i£ 

P5     fa 

03 
Pi 

1 
- 

- 

9 

go 

= 
— » 

3? 

-: 

1 

B 

cn 

0 

- 

00 

_c^ 

2 

1 

£ 

E 

s 

— 

% 

— 

a 

x  a 

X 

0  0 

s§ 

X 

0  0  i> 

X  S3  c 

c 

p 

8 

1,202 
1,114 
1,058 
L192 
1,112 
947 
092 

— 

93 

NCNNNNN-lNNNfJNL«r: 
C  ?)  ■-  l-  r  -  X  M  -  N  X  Z  ?  -  :: 
<M~HOOOCi-.otoi-~Trco  —  orr.  cr. 

705 

629 

1, 075 

013 

1,212 

1,044 

NNN3CN-L«CL:or; 
OrCJC-iL-X-^rT 
OSOXXNCi- <  O  OJ  O  tO 

000 

1,199 

1,005 
1,035 
1,  195 
1,048 

X  eg  N  x  x  re  x 

go  x  —  0  x  «  0 

CO  O  CO  OO  CO  CO  COO  CO  CO  CO  OO  OOtOt-- 

■a  —  l~  t^  x  to 

0  r»  cs  l-  x  10 

NX*  XSN* 

GOXXCNSOt-L~Oi-~ON- 

COC3*T ■-  —  -o  l.- 

COSSNXrtrCCX 

900 

301 

486 

405 
305 
452 

SSSSSgS 

DO 

SS^^SSSS  i^SfeSU 

— 1  CN  to  "<*  l~  JN 

T7  TT  ,r  Ifl  SO  * 

O  C  N  cr.  O  *  CT  l.-  X  l~  CO 
N*0        i-(        COM         »-i  SO 

3S3S23 

815 
903 
959 
820 
900 
1,065 
1,320 

X 

09 
BC 

750 

897 

950 

905 

1, 070 

1,100 

1 ,  330 

1,398 

1,500 
1,510 
1,030 
830 
920 
1,047 
1,079 

N  r:  N  r  c  r; 
c  x  r:  c  r.  ■-: 
M  BC  09  SONC5 

1,  015 
1,005 
1,  115 
1, 199 
1,  290 
1,354 
795 
910 
1,025 
1,040 
1,337 

1,380 
770 
910 
940 
817 
964 

1 1 


—  CN 


£0 

3  M  a  '-> 


—   Qi 

7:   ~ 


S3  S3  •  5   £    5    ^ 


- 

S,  . 


C5  09 

ii 


—  ^-^^ 


25^     ^& 


:z~5z^-  :r^^ 


^ 

i: 

pq 

PP 

pQ 

X 

PQ 

pq 

pq 

N 

C<1 

ri 

?j 

CN 

a^ 

X 

kS 

428 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq— ^onpoid  ps^rai 


■;90j— q^dep  ib;o  j, 


•^aj— mdepno 


83 


•©id 


to 

T 


ran^p  8AoqB  apnmiv 


r^I^t-»00t^CNir~t^l^(NT-<T-l5O<O< 


lOOHHHOOtDHrt, 


'MOOIOICO' 


•^aaj— pA9t 


i  00  00  <N  CO  CO  • 


nOiCKONOOMOrt' 


1-^1  03  05  OS  "31 

ihiNOtpN 
i  •'Ji  Tti  io  io  M 


pa^j^onad  ssau^otqj, 


'cSS' 


•^aj— d<n  <n  q^dea 


lOHHCOfflNl 
lO00«OH(N! 
I  CO  CO  CO  lO  SO  05  < 


lOMiONOOooiOOeo 


bO 

-O  o  o 


-tf(£ 


Mm  : 


C3  C3      ■  O  O 

flpl.'pp 


03  O 

id  ? 


-dTd-^'d  3  So-53-3  2  o'C^  3-^  ^'n^^^Td 

:  :  :  :pqpq-  MM^Sw  ipqW^m  :  :  :  : 


§5 
MM 


3  %2  ?  S® 
d2«2  «  ^.2.2 


.-<        o 


o 

o 

o 

o 

o 

o 

=3 

4 

°3 

g 

fl 

.S 

^ 

^ 

^ 

*< 

3 

«! 

S 

H 

5 

o 

o 

u 

S£ 


BLATCHLET] 


TABLES    OF    WELL   DATA. 


429 


(N      . 

a  : 

C3    . 

|  : 

M    ' 

§  : 

_.   <D 
'O  © 

(A 

a? 
<2 

as 
Is 

a 

s 

_a 

© 

EQ 

c3 
0 

03 

- 
C3_ 

1 

'eS 
0Q 

? 

en 

o 

+3 

S3 

a> 

to 
o  a 

m 

,i 

c 

:: 
w 

c 
- 

a. 
PS 

r 
— 

n 

l 

43 
O 
0B 

© 

g 
03 

QQ 

O 

.a 

.a  .a  .a 

60  60  60 
'333 

■4-a 

•a 

'3 

a> 

tO 

M 

■Q1    O 

oo 

3 

§ 

to 

M 

I 

5 

8§ 

cot^ 

1 
as 

CO 

-*  r~  (M  »O-00 
00  •*  tO  ■"»<  OS 
C^OOOOOSCN 

oiom 
oo  as  o 

tO         HO00NM         -^f^lO 

<m      oocoasiOTji      omo 
as      as  as  as co as     oaso 

(ONHOt 


■  OS  l>  to  U5  t 


I  OS  CO  CM  CO  CO  "-    — 

irH'JDNOSOOOJMtOOSHOSOO- 
OtOWHOOlHOfflOlNf     ■ 


CO  t*i  (M  OS  CO  OSCOr- 
O^00C0"O  OOcOOS 
O  O  OS  to  O       as  O  OS 


NMOOOO         lOWOOWlOlOOlOOOONCCOO'HTl'OOr-NOOMMM 
OCOOOVN         OOtOTfOm^OCtHDWMOWCRWMMOHOOOMOOO 

coco^cocoti      ior^oococoTt<ioiot>-ooascoeoco'«j<oo< 


lOCO-^'O'Ot^t^OOCO'ti 


r~toootot*-      hnm 

OJO^H*  HMO 

•^TptOOOTjl  lO  ■*  lO 


MONHI 
CNrHIMCO' 


:ss 


to  to  Tji  lO  O  lO 

r^  o  t- r^  cm ->s<      to-<j< .  . 

t^  oo  oo  t»  oo  as     o  cm  co  t^  oo  as  as 


OlOlOOOOlOOMlOD.NIML'JOONHHOlNlOmiOOOrtMOO         HON"00 


"d  o 
PQ  : 


C3      •  O  © 
fl     '  o  & 

2~to  *  §> .  .  . 

"§  cS-^Ti  O  O  O 

PQ3  Wea 


s    fe  >>03 
ot  r  03  6o 


o  o  o 
o  o  ft 
fe  fe  © 

izjr:<i^oA).     .     .p'^&o.     . 

O  •"  2  'C  ^  T3  -a  .5a  .a  "S  -a  -a  tj 

:eq2  Whb  :  :  :WWm  :  :  : 


a 

a 

c5 

'O'd  3 

:  :m 


:  a 

X  — 


O  Oa    . 

*8>  : 

Mx>  o 
•5a  -C-O 

Mm  : 


O  O  O^' 

«t3  -a  .5a  • 

:  :  :Wi 


o 

o 

o 

o 

o 

o 

o 

O 

O 

Q 

o 

O 

«a 

<% 

^5 

■8 

•a 

4 

a 

0 

fj 

.3 

a 

a 

m 

M 

44 

m 

^ 

M 

< 

< 

<4 

<! 

«j 

< 

.22 

3 

5a 

3 

s 

3 

a 

o 

O 

O 

o 

o 

430 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•sjajxeq— pnpoid  roprai 


•paj— q^dep  psjoji 


•paj— q;dop  no 


;aaj — aireid 
mrn'Bp  9Aoqe  epn^i^v 


•}99J— I8A9I 

■B9S    Avopq   epmpiy 


•}99j— 
pg^j^guad  ssgn^oiqj, 


•180j— do^  0;  mdaa: 


as 


g  . 

02 


CD        '+S 


OO 


C3  Tji         l^OlNNOONOlO<»OHOOONOOHT)(NOI'-N(Ol'»Mf3NOa 
1-IO  OlfflCOin^^MHO)HHHINOOJ01N<0!OlOHO*lOHHOtO 


1000000)OOHC010COMMN1'IOIONOOOOO)C<5'*OOOVMC01<( 


!8S' 


tj-CN  CN      ■««« 


1  »-i      inoiotofflinooiiosdicoiooooooMONcqfHTfiTfN! 

10       hO<0hO(DO00hnONNO01(0NOOOOhOO^<0W( 


0 

0 

0 

fc 

fc 

fc 

§, 

& 

ot 

1 

.a 

.9 

"3 

3 

X 

m 

CO 

c     a  a 

9         9  9 

MM  M 

3    »a  3 


i- 


BLATCHIJEY] 


TABLES    OF    WELL    DATA. 


431 


tc 

! 
8 

So 

*2 

9 

8 

3 

- 

Gas 

Oil 

Gas 

Oil 

1 

= 

f 

oo 

c 

O 
IC 

3 

0 

•  - 
CO 

8 

CO 

en       oo 

c3       O 
O 

s 

1  - 

OS 

1 

i  - 

s 

1    S 

S 

£ 

3S 

as 

M 

OS 
CO 

>o       CO 

" 

2. 

s 

at 

s 

r 

a 
— 

-- 

K 

- 

CO 

— 

gSSKS? 


So 


O  O  O  =0  O  -«9«        ooo 


j;  M  M  n  •*  l-  t^ 
0NOCOOOOC4O 


IONS    .  _ 

OC^OrHOl-^OOOl-H 


Tfr^C^TfOOlMlMOOCJO-^'Ci- 


'  O  OS  iO  lO 


■  ■^J1TI<^-.oooO'^l'^'co■^r'^,• 


«Nrct;r:-t^;cS-rN^NX-HO'rXO-i-r«-rOL':j;^cito       .-n^oOi-- 
Tj.rj.TTTr^-Trt^^rr'r-r^ooooooco-^^cscoi-'soocooOco^csioooiO      oo  cm  co  oo 


OOTOOOOiOuOOO-w-^OOOOiO 

CO  ^H  CO  CO  rttOHLIWttJlOH 


—  —  -~  —  oa  tc  x  eo  re  oo  — •  r--  c<)  co  so 
3JOi«cocoo>Oiooaoo5aaosco'*>o 


OKOC  ifl  DC  NOOlQXMO  1Q  XtrOHLK 
■Trt^5--XC-Cr)X^-r-HCCC;»?J»'<f! 

99  aa  3-.  «  a:  a-,  cs  co  i-  93  m  co  co  co  t-  oo  as  t^  oo  i 


>  co  oo  co  oo  as  t^>  < 


u 


•oo 
'  o  Q< 


:5_  £ 


Si. 


I'W  :  o 
•'  8  §  J  a 

.„       -*       >      ©      6X) 


TnilSSs 


-aoooocd^Tlos^U'dooo 

q  :  :  :  :  :;  ^a  :-  M^hs  :  : 


c3  O 
fl  O 

-d  3-5 


a5  & 
®  te  © 

•d-g-d  o 

awn  : 


5 


°  2 

O  P-i 

5»   he 

^d  o^ 

.s  -n  x!  4s 


•S      .S 


o      o      o      o 
&     fc     5?     fc 


ooo 
J?  £  £ 


C        fi        e        c 

c3  c3  c3  c3 

£       £       £       £ 


X3      XS 

o    o 


o    c 


ooo 

2  2  2 
ooo 


432 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq— :ptipojd  veiimi 


•188j— mdap  leioj, 


laaj— q^dep  no 


•a 

a> 

.2 

o 
U 

I 

ft 

«0 

Eh 


umi'Bp  aAoqB  apmi^Y 


•;88J— I8A8J 

■B8S  A\opq     epn^T^iv 


pe^Bj^sned  sseu^oiqj, 


•;88j— do^  oq.  q^doa 


i  •  x  .    I . 

da  .2  ©  >.2. 


ft  • 


CO 


8        £?£> 


«      i 

fc    : 
eh    £b 


A        ft 


t-<  CM  l-H 


1CIO        ©  ■      'NN 

S3S    S      :  :3S 


«.  — •  ^  £3      °°      o  cm  co  c 

iffliOffiffiHO        00        ■>*  t^  lO  CM 
lOfflHONH         CM        CMCM-cHCM 


ooaoinmcote      cm      o  oo  r^  cm      io 

OWlOOOOOCJ         r-l         tDIN^H         CO 
CO -cf  00  CO -<T<  CM  CO        CM         CM  CM  O  CM        CM 


cm  cm  2  cm  cm  cm  2 


CM  •>*!  00         CO 


(ONNNlOOin         t-         CM  CO  CM  (^         O 

^H^Ci-^TfiCMCO    -^    Ci  CO  00  "^<    t^ 
00  CI  CO  00  Ci  CO  CS    CO    CO  CO  -<Ji  CO    CO 


h3  o 


°  s 

O  ft 
&■  tuO    . 

Mpq   : 


:  ^  o  o 

,2 ,2  £3  6 

'O'O.a  o  o 

:  :M2  a 


IOCO  o 
lO  U3  io 


ooo 


lO  O  CM  CO  00 
O  rH  O  O  I— I 


'OOOOt^ 

■  ^COOIH 
lO"**  Tf  CO 


iocoo    .  r» 

Tf  Tfl  CM        •  ■** 

lO  lO  lO     ■  co 


"ffiCSCNO© 


CO  COCO  •"*<  CO  l 


Oi-HO  t^< 


CM  lOCO  OCO  lO 


:S 


CM     CM 


CO     00     CM 


o    o 


3  3 


6£   £ 

-~®    © 

»9  3 

So    o 
to  to 

JSP  5? 


o      t^    ic 


£  fc 


bX)      S3    13 


IN     H     N 


r££ 


T3    -O 

ft  ft 


<tj     fi   Q       fl     Offl 


fc  B  £ 


coPm 


^  J3  XJ 
o  o  o 


■g 

o 

£.2  .2 
Wo  o 


o    o 


2  22  2    2  .2 
2222  2  2 


MM        W      OOOO    O    O 


CO     ■<*>     IC 


CO  r-H  l-l  T-H      CM 


iiOOf-     00     Ci 


H 

i* 


z;  .^  . 


BLATCHLEY] 


TABLES    OF    WELL    DATA. 


43a 


co  us 


s-   03  t-   O 

IQOQ2 


i— I    C3 


olgol 

o£o 


s  :§ 


3  „ 


111' 

c3  o3  ®' 


COONOiOi 


g    •  >, 


»0<OOMO"5<0 
CD  lO  iO  C-O  iO  ^O  iO 


ocn^HMioN 

•^-^i-^it^cO-^CO^n 

toiooooioioin 


JcaOOtOiCHCO'i'lNlOOOi-KOcO 
iCOOit^O.  OiCJiCOt^air^OOr-ieOiO 

'cocsco<Mcococococococooa>co 


r-  Tf  eji      <N 


I  CO         C5  00  < 


<»HOO'»oa:NS30oocS'j''* 

XMHMOOOMNOINH00O'* 
OHNi-itNHHHHHHrtlJtlOX 


i  oo  oo  co  <— i  co  co  i— i  r^  Oi  co 

lOXONONOHOH 


tocsaoHNcji 


cm  irj  t^  t 


lOJiHHrl 


lOONH      .  (M      .t35      .O 

•^^i>co    -<N    -es    .co 


iNtOtBOOiOMHMOMOOO 
ICOftO^^^NO-itiffl^NOOO 
iO(OiO!OloioiOiOiOiOi0050N 


Old        lOOOOOMOMiOrtiol 

»-H  i-H  COCOCJtXl^r-lTUHMHI 

O  CO        0>ON'*COiO<OiO®K5i 


(OffiHMTriO! 


-to"  to*  J? . 

«  o?§  &>o  &  . 

SSoSo^oooooo'Oo'S 

ft  ?3T3'Cd'OT3''d'£rd  3 


hhS^§£ 


"is      C^ddo^  "3  "^  "**< 


^  o 

&8f 


H^W  £ 


ill 

~  i  s 


2  o-as 


M 

«  §  8  -■ 


CO     lO  CO  CO  iO  uHC  «3 
CO      CO  CO  CO  CO  CO  CO  CO 


CO     CO     CN 
CO      CO      CO 


£  52  ■ 

.2     JSJSO  OOO17 


glg.2f  I 

ZOhPhQ    ^ 


O  OOOOO  O 

fc  2   2   2  2  £  2 

_Cj  c3        c3        c3      03      c3  "c3 

"3  "3    "3    "3  "3  "3  "3 

2;  2;     2     55  £  2  2 


.2      .2  .2.2.2.2.2.2.2     "o    -a.0 .2  >> 
,c     2  £252222    *c    'n22  e?  03 
o      o  OOOOOOO    cq    pqooW  S 


1 

OS 

0 

S-i 

A 

O  t-h     CNMHlNM^rt 


COr-HCM  CO 


CO        Tt>     O 


-28  G 


434 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


•spxreq— pnpojd  p3ijnii 


•^aj— q^dap  p^oj, 


O  CO 

3S 


a 


•CO 

28 

g 


i 

s 


•;aaj— qjdap  no 


SIHHH 

lOOtOtO 


ran^Bp  OAoqe  apn^t^v 


<M        00  Oi  C  05  lO  (N  O 


HOfflfflN^'WOOtDOO'V^pHCOlOnWW 
000«5NCON-*COiOO^OP5N(NiOm«HM 

lO^fi  coco  coco  Ttico-^-^-^'J'ooM'cc'*  coco  *n 


•^88  J— \9AQ\ 

eas     A\xqaq  epn^ptV 


tp  Tti  CO  oo  io  r-  o 

OXOlOOHM 


©,-i,-It-Ii-i©i-iO©©i 


i00NT|<tO!O00ffi 

I  O  T-H  O  T-l  i-H  O  — 1 


pa^i^aiiad  ssau^oiqj, 


O'0HO'*MNMi0NNOO< 
fflCOiHfHCOHCCNHHrtC^COi 


o5cocoi-ics 


'laaj— doj  o;  qidaa 


00C«3O)MOHrt(X)( 


>•  = 

<*  P. 

a>,2  tuO 

go's 
C5~ 


rH(Nrt(N 


Sl|f^- 


M 


3g-2  ^3® 
co«2  «  >.2£ 


CO         CO      CO      CO 


oo  i± 


ftp,  °^ 
UP  £ 


OJarj    Q      Q- 


O  H  <N 

^  6  d 

of  fc  fc 

•—  00  oc 

H5  "3  'S 

od  £  £ 


P4     * 


•«  o 

CO 


-Cfl 

C3 

c3 

03 

^5 

£ 

-C 

— 

CO 

DQ 

OO 

w 

a 

ffi 

O 

O 

O 

2 

OS 

O 

Hd 

M 

<* 

«« 

CO 

t- 

X 

~ 

BLATCHLEY] 


TABLES    OF    WELL    DATA. 


435 


!  <2<£ 
'20O 


be"* 

fli-T 


QO 


EC  ^> 

^8 


■2— • 

3"3 

+3    ® 


N  N  N 


-^<   -*l   -»l   •«<  T}< 


—  r  i 
co  go 


00  iO      .CONOU5 
Nh      iOCOOh 

co  co     ■tcmtp'* 


r^;OoOTf<r^f»coioC300''Wi-icJjao 
->3<cO''tf|co'OTr'co>-';cocOLO,co>0>o 


.-  —  - 
co  —  V 


I-  to  CO 


OiHK  —  lO  H  C  O  -  t^  I-  N  C  X  K  i-  ;  iC  iO  X  73  CI  M  <t  O 
'rtL'5NU3  0>NrtNMfflC!H-H3rt3MOflv0MC0l0e0N 
!C»XN»»OLTL-cr.  00  —  lOiQOOOI-tOiO  «o  O  O  iO  o> 


os  co  oo  so  oo  ec  • o  r.  to  x  -/)  c  ^  ■* 

©i— t  ©  i-H  Oi  O  *— <  Oc  t— iHOii- i  00  © 


"-  60  -r 

©•a  — 

03  OS  lO 


cm  t~-  tp  -^  as  t—  as  ■ 

©  as  ■*  T  to  to  t^  : 


iCNClKOMOXOMCKXCSNntStOmtCOO 
IOOX5!»^COX'»0'T!Ol-MM3SC»OiC!0 


ONNtDOOHgOOiQONlON 


S38! 


ncl-cxml-cc;cmco;oxo    iSononcs^oio 

CM         t-ltO         (OMrtHHM^CM^-rt-i  .  O  — 1  CM  CM  —I  .-H  -*  ,-(  ,-♦ 


O  W  O  00  CO  O 
uO  (^  co  t^HN 
.-I  CM  CO         CO  ■<»<  00 


OiOCOiCOiOtOtOSXOOoOuOCMCMOiOOOt^-CMCMCMOiO 

CM  Ci  r*  '00  •>*  tO  CM  to  O i  «C  CO  --I  CM  f-  CO  t IMHCOOOOOH 

O5©-H^HCNCNC0CO-*<X©rtCO  CO-^'X^CMCOCO-^'-^'CO-*-^ 


C  -  X  M  C  O  C  ?.  ic,  O  O  M  ID  X 
KOHONI-snOOMOOl^ 
uO  to  lO  to  ^r  -r  CO  ^r  to  to  tji  to  "^  CO 


hNC 

:_-  r.  ■_- 


IS    «■  • 


53 
5  & 

P  fcX) 

-44-9  c 


CNCO 

la 


rt  cn 


:cq 


OOCSCS 


i  CM 

■  o  g  ce 
P  £<£ 

r*  ^3  o  ct3  c3 


13  T3  T3 
o  o  o 

Q  0  O 

MMM  :  :  : 


N     CO     f     X     V 


""3"      CO 


to  r--  to  to 

coco  coco 


c 

cs 

6  £  6   «  ^  u°  ®   ^£532 

£  e.  !5    e  d  d  6    ^  »  .* . 

■3  1  -g    £  £  £  £    £WWWS 

m  P.  m  15  -3  -3  3  -3  Jl  S  J 

§  £  s  £  £  £  £  £<<<< 


dod> 
ooo  £f 

.  .  .  s 

OCOJ 


.2  .2  .2  .2  2 
2  2  2  2  2 
o    o    ooo 


.2  .2  .2.2.2.2  2 
5  2  22222 
o  o  ooooo 


2  o  o  o 
2222 
oooo 


i-l         CN      CO      -S"      tO 


436 


OIL  FIELDS  OF  CRAWFORD  AND  LAWRENCE  COUNTIES,    [bull.  no.  22 


O 


w 
M 

£ 
o 

Pi 

4a 

£ 

o 
E5 

3 

O 

•  oj  OJ 

•(MOO 

'OOl 

;  to  -*1 

03 

0 

CD 
03 

0 

•qauBq— ;onpoad  \m%mi 

SSSb  : 
o    o  : 

-O      ■ 

00    . 

CO 

'%Ml— mdap  iB^ojj 

i 

OO     • 

i  : 

•*i  CO       • 

©to    • 

to 

■%d*j— mdap  no 

. 

O 

i 

55 

0  • 

tOtO     • 

toto    '• 

0 
to 

OQ 

mn^p  8Aoq«  apnmjy 

00IN«CO-HTl<-HNO5M 
TfOOCOtriOO'S'COCO'^CO 

•;88J— I8A81 

B8S   Avqpq   apnmiv 

OhhohOhhoh 

•^98J— 

•OOXNiOO 

•  CN1  i— 1  r-<  r-i  r-i 

•^88;— doj  oi  mfoa 

0>-ie<100tOiOcoa5iotp 

LOHoa-iO)HO'*o 
•*  (O  to  ^  O  •*  ©  to  ■*  to 

E 

03 

o 
©■ 

»    1 

2  £ 

3  :m 

-5 

3  :1 

0 

Sur- 
face 
ele- 
va- 
tion 
feet. 

iO     O     iO        O     to     00 
CO      CO      CO         CO      CO     CO 
TJ1       Tf       -<J1          V       ■*       t 

Name  of  well. 

CO 

c 

a 

c 
a 

- 

C 

c 

■   1 
c 

(J 

c 

.  1 

c 

c 
ft 

>    c 

5  x 

-'.  > 

1  f 

12 

c 
c 

e 

i 
i 

*> 

3 

3 

Name  of  oil  company. 

.2  .2  .2    .2  .2  .2* 
'23  15  5    5  2  2 
000    000 

C3  O 

w    n   ■*      10   to    t>- 

g  . 

•j3  o 

CO 

CO 

437 


INDEX 


A 

PAGE 

Abandonment  of  wells  in  Illinois 181 

Accumulation  of  oil 16, 18 

k  Under  impervious  cover 22 

On  LaSalle  anticline 143 

In  Robinson  pool 104 

Ackman,  pumping  station  at 164 

Acknowledgments 12 

Albion,  prospecting  near 16 

Altitude  of  sands,  method  of  determining 95 

American  bottoms,  prospecting  on 16 

Annapolis,  gas  sold  to 181 

Anticline,  definition  of 22 

Effect  of 83 

In  Buchanan  sand 108 

In  "Gas  sand" 109 

In  Kirkwood  sand 110 

Anticlinal  theory,  confirmation  of 11 

Arches  in  Robinson  pool 99 

Areal  extent  of  oil 12, 25, 27 

Of  oil  1  and  in  states 145 

Production  of  oil 163 

Armitage  No.  2  well,  record  of 123 

Associated  Producers  Co.,  pipe  lines  of 166 

Aviston,  prospecting  near - 16 

Axis  of  Illinois  basin 142 


Bailer,  description  of 154 

Bailey  pumpmg  station 164 

Bain,  H.  Foster,  general  sections  by 26 

Bakers  Lane,  loading  racks 158 

Band  wheels,  use  of 152 

Bartelso,  prospecting  near 16 

Barren  wells  in  Illinois , . .  145 

Base  map,  use  of 96 

Bellair,  gas  areas  near 181 

Benoist  farm,  prospecting  on 15 

Sand,  correlation  of 109, 182 

Big  Four  Oil  Co.,  development  by 106 

Birds,  gas  sold  to 181 

Loading  racks  at 158 

Boiler  house,  use  of 158 

Bolton,  E.  C,  work  of 164 

Bond  County  sand  correlation  of 109 

Bonus  for  oil  leases 147 

Bowers,  J.  D.,  No.  7  well,  record  of 129 

Boyd  No.  11  well,  section  of 119 

Bramsky ,  Oscar  E . ,  investigations  of 20 

Bridgeport  gas  areas 181 

Loading  racks 158 

Pumping  station 164 

Tank  farm 165 

Bridgeport  Oil  Co.,  development  of  Bridge- 
port sand  by 106 

Bridgeport  sand 15 

Correlated  with  Pottsville 83 

Cost  of  drilling  to 153 

Depth  of 106 

Development  of 106 

Distribution  of 106, 137 

Drilling  of 154 

Initial  production  in 137 

Production,  rank  of 135 


PAGE 

Production  of,  in  Bridgeport  Township. ...  137 

In  Dennison  Township 137 

In  Lawrence  County 106 

In  Petty  Township 137 

Salt  water  of,  in  Dennison  Township 141 

In  Lawrence  Township 140 

Stratigraphy  of 106 

Thickness  of 106 

Type  area  of 137 

Bridgeport  Township,  wells  in  Kirkwood  sand  137 

Gas  in 108, 139 

Gushers  in  Buchanan  sand 137 

Production 135, 137 

Salt  water 140 

Structural  relations  of 137 

Type  area  of  Bridgeport  and  Buchanan 

sands 137 

Wells  in : 135 

Brown  &  Hogue,  purchased  by  Ohio  Oil  Co. .  163 

Buchanan,  R.  O.,  farm 107 

Buchanan  sand 15 

Anticlinal  dome  of 108 

Cost  of  drilling  to 153 

Discovery  of 107 

Gas  in  Bridgeport  Township 139 

In  Lawrence  County 107 

In  Petty  Township 136 

Production  of,  in  Bridgeport  Township 137 

In  Dennison  Township 138 

Salt  water 107 

In  Bridgeport  Township 140 

In  Lawrence  Township 140 

Structure  of 107 

Tvpe  area  of 107, 137 

Bull  wheel,  use  of 152 

Bureau  County,  gas  in 182 

Burton  Bros,  development  of  Kirkwood  sand 

by 109 

Busch  and  Everett,  development  of  Tracey 
sand  by Ill 


Cady,  Gilbert,  work  of 28 

California  oil  land 145 

Campbell  Hill,  prospecting  near 16 

Capillary  action 19, 20 

Carbondale  formation  in  Crawford  County  ...  53 

Stratigraphy  of * 28 

Carlinville,  gas  near 183 

Prospecting  near 15 

Carlinville  limestone,  correlation  of 53 

Carlyle  oil  field,  description  of 16 

Oil  prices  in 169 

Carlyle  sand  correlation  of 109 

Carter,  L.  D.,  prospecting  by 14 

Carmi,  prospecting  near 16 

Casey,  gas  sold  to 181 

Loading  rack  at 158 

Pumping  station  at 164 

Casey  pool,  development  from 146 

Casey,  sand,  position  of 29 

Casing,  use  of 155 

Weight  of  per  foot 160 

Central  Refining  Co.,  Perrv  King  No.  5  well..  12s 

Refinery  at  Lawrenceville 16 

Tank  car  shipments  of 166 


438 

Index — Continued. 


PAGE 

Cerro  Gordo,  axis  near 142 

Champaign,  gas  near 183 

Champaign  County,  prospecting  in '. 15 

Chester  formations,  description  of 30, 31 

Distribution  of 31 

In  Lawrence  County 83 

Kirkwood  sand  in 84, 109 

Limestone  strata  of 83 

Red  shale  in 84 

Salt  water  in  Lawrence  County 140 

Top  of 29,  82 

Childress  No.  3  well,  record  of 78 

Christian  County,  gas  in 182 

Circulation  of  oil 18, 20 

Clark  County,  acreage  drawn  on  by  oil  wells  .  151 

Cost  of  wells  in 153 

Gas  sand  in 182 

LaSalle  anticline  in 142 

Production,  daily 163 

Prospecting  in 12 

Storage  tanks  in 165 

Clapp,  Frederick  G.,  classification  of  structure 

by 23 

Coal  fields,  selection  of  well  sites  in 151 

Cobden,  prospecting  near 16 

Cochran,  C.  T.,  No.  9  well,  record  of 51 

Colchester,  gas  near 183 

Columnar  section 84 

Of  Crawford  County 33 

Of  Lawrence  County 54 

Contour  lines,  use  of 11, 12, 96 

Of  Robinson  sand 99 

Of  Honey  Creek  pool 99 

Contract  for  drilling 151 

Cornplanter  Refining  Co.,  shipments  of  . .  .166, 169 
Correlation  of  Benoist  and  Kirkwood  sand. . .  182 

Or  Bridgeport  and  Pottsville  sands 83 

Of  Carlinville  limestone  53 

Of  "  Gas  sand" 108 

Of  Kirkwood  sand 109, 182 

Of  Robinson  sand 98 

Of  Bridgeport  sands 82 

Cost  of  drilling  wells 152, 153, 160 

Of  operating  a  lease 161 

Coulterville,  prospecting  near 16 

Crawford  County — 

Acreage  drawn  on  by  oil  wells 151 

Carbondale  formations  in 53 

Columnar  section  in 33 

Cost  of  wells  in 153 

Development  in 14, 146 

Drift  in 52 

Extent  of  pools 97 

Gas  sand  and  gas  pressure 182 

Geology  of 97, 142 

McLeansboro  formations  in 32, 53 

Pennsylvanian  rocks  in 53 

Pleistocene  in 52 

Pottsville  formation 54 

Production,  daily 163 

Prospecting  in 13 

Shallow  sand  in 99 

Stratigraphy  of 32, 52 

Structure  of 99 

Storage  tanks  in 165 

Crawford  County  Oil,  Gas  &  Coal  Co.,  work  of    13 

Cross-section  A-A 114 

B-B 123 

C-C 125 

D-D 130 

Cross-section  of  Lawrence  County 114 

Cross-sections,  use  of 11, 96 

Method  of  construction 114 

Cumberland,  pumping  station  at 164 

Cumberland  County,  production  in 163 

Gas  found  and  gas  pressure 182 

Cummings  No.  12  well,  record  of 70 

Curtis,  C.  F.,  No.  8,  well,  record  of 44 

Curtis  &  Aiken,  record  of  Fitch  No.  17  well  . .  119 
Cypress  sandstone,  unfavorable 31 


D 

PAGE 

Duncanville  pool,  development  of 14 

Day,  Dr.  David  T.,  investigations  of 20 

Oil  statistics  compiled  by 167 

Decline  in  shallow  fields 163 

In  Illinois  fields 181 

Decatur,  prospecting  near 16 

Dennison  Township,  best  wells  in  McClosky 

sand 137 

Drift  in 82 

Gas  in 139, 140 

Kirkwood  sand,  most  productive 137 

Production  in 135 

Production  of  Bridgeport  sand 137 

Of  Buchanan  sand 138 

Of  Kirkwood  sand 138 

Of  Tracey  sand 138 

Salt  water  in 141 

Structural  relations  in 137 

Type  area  of  Buchanan  sand 107 

Wells  in 135 

Denny,  prospecting  near 16 

Derricks 152, 153 

Derry  Township,  prospecting  in 13 

Deuchler,  W.  E.,  work  of 12,94 

Development  of  oil  properties 146 

DeWitt  County,  depth  of  gas  and  gas  pressure  182 

DeWolf,  F.  W.,  work  of 28 

Diatoms  as  the  origin  of  oil 17 

Diffusion  of  oil  through  rocks 17 

Through  Fuller's  earth 21 

Dip  of  Buchanan  sand 107 

Of  Kirkwood  sand Ill 

Of  McClosky  sand  on  LaSalle  anticline 114 

In  Petty  Township 113 

Of  Robinson  sand 100 

Dome  Structure 83 

Of  Buchanan  sand 108 

Of  "Gas"  sand 109 

Of  Kirkwood  sand HO 

Drake,  J.  M.,  No.  23  well,  record  of 47 

Drift  gas 26, 183 

Drilling,  method  of 154 

Cost  of 153 

Drive  pipe 155, 160 

Drole  No.  7  well,  record  of 117 

Dry  spots  in  Robinson  pool 100 

Dry  holes  in  Illinois,  table  of 180 

Duncanville  pool,  general  level  of 100 

Price  of  oil 167 

DuQuoin,  prospecting  near 16 


East  St.  Louis,  refineries  at 166 

Economic  features  of  Illinois  field 145 

Edgar  County,  daily  production  in 163 

Depth  of  gas  and  gas  pressure 182 

Edwards  County,  in  Illinois  basin 142 

Edwards,  O.  F.,  No.  15  well 35 

Efficiency  of  gravity  system 165 

Of  Illinois  operators 145 

Eldorado,  prospecting  near 16 

Ellis,  J.  R. ,  work  of 91, 93 

Eshelman  No  7  well,  record  of 129 

No.  16  well,  record  of 129 


F 

Finley,  D.  T.,  early  work  of 14 

Fitch  No.  17  well,  record  of 119 

Flat  Rock,  gas  sold  to 181 

Flat  Rock  pool,  correlation  of 14 

General  level  of l°y 

Fuller's  earth,  diffusion  through 21 

Fusulina  fossil  as  a  marker 28, 33, 44, 53 

Fyffe,  E.,  No.  29  well,  record  of 126 


439 

Index — Continued. 


G 

PAGE 

Gas,  areas  of 118, 182 

Depths  of •. .  182 

Gravitation  of 22 

In,  at  or  near: 

Bridgeport  sand 140 

Bridgeport  Township 139 

Buchanan  sand 139 

Carlinville 183 

Dennison  Township 140 

Drift  formations 26 

"Gas  sand" 139 

Jacksonville 183 

Kirkwood  sand 139 

Lawrence  Township 140 

LaSalle  anticline 143 

McClosky  sand 139 

Morgan  County 183 

Pettv  Township 138, 139 

Robinson  pool 99, 103 

Tracev  sand 139 

Pressure  of 20, 182 

Production  of  in  Illinois 181 

Gas,  sold  to: 

Annapolis 181 

Birds 181 

Bridgeport 181 

Casey 181 

Flat  Rock 181 

Hutsonville 181 

Marshall 181 

Martinsville 181 

New  Hebron 181 

Oblong 181 

Olnev 181 

Palestine 181 

Pinkstaff 181 

Porterville 181 

Robinson 181 

S  toy 181 

Sumner 181 

Vincennes 181 

Westfield 181 

Structural  relations  of 138 

Use  of 147, 181 

"Gas  sand,'-'  absent  along  D-D  cross-section. .  130 

Anticlinal  dome  of 109 

Correlation  of 108 

In,  at  or  near: 

Bridgeport  Township 108, 139 

Lawrence  County 83, 108 

Marion  County 182 

Petty  Township 139 

Sandoval 182 

Structure  of 109 

Thickness  of 108 

Gas  wells,  price  of  per  year 147 

Geological  sections  of  central  Illinois 26 

Of  southern  Illinois 26 

Geologic  structures 22 

Georgetown,  Ky.,  Indian  Refining  Co.,  at 166 

Gillespie,  E.  X.,  record  of  Smith  Xo.  24  well .  130 

Gilpin,  J.  Elliot,  investigations  of 20 

Grades  of  oil 167 

Grafton,  prospecting  near 16 

Gravitation  of  oil,  gas  and  water 22 

Gravity  lines  to  leases 164 

Gray,  W.  B . ,  record  of  No.  2  well 63 

Greenville,  correlation  of  sand 109 

Gas  area  near 182 

Prospecting  near 16 

Griswold,  W.  T.,  theories  of  oil  accumulation.    24 
Gushers  from  McCloskv  sand 135 


Hamilton  County,  Illinois  basin  in 142 

Hansen,  prospecting  near 16 

Hardinville,  gas  areas  near 97, 181 


PAGE 

Hardinville  quadrangle,  description  of . .  .86,87,91 

Hey  worth,  drift  gas  near 183 

Henry  Xo.  1  well,  record  of 133 

Herrick,  prospecting  near 16 

Herrin  coal  and  Carbondale  formation 28 

Hoblitzell,  J.  J.,  work  of 14 

Honev  Creek  pool,  opening  of 14 

Structure  of 99 

Hutsonville,  gas  sold  to 181 


Illinois,  natural  gas  in 181 

Wells  drilled  in 145, 181 

Rank  as  a  gas  state 181 

As  an  oil  state 145 

Stratigraphy  of 25 

Structure  of 32 

Illinois  basin,  axis  of 142 

Illinois  oil  fields,  efficiency  of 145, 146 

Extent  of 145 

Saturation  theories  for 24 

Impromptu  Exploration  Co.,  prospecting  of. .     15 

Independent  oil  companies 166 

Indian  Refining  Co.,  operations  of 163 

Initial  productions  in  Illinois 101, 135, 180 

Of  Kirkwood  sand 109 

Of  Robinson  sand 101 

International  Oil  and  Gas  Co.,  development 

by 112 

Interval  between: 

Buchanan  sand  and  " Gas  sand" 108 

Chester  and  "  Gas  sand" 83 

Kirkwood  sand  and  "Gas  sand" 110 

Kirkwood  and  Tracey  sands Ill 

Tracey  sand  and  Chester 84 

Tracey  and  McClosky  sands 113 

Investments  in  oil  properties 162, 163 

Iola,  prospecting  near 16 

Irick,  William,  wells  of •  13 

Iuka,  prospecting  near 16 


J 

Jacksonville,  oil  and  gas  wells  near 183 

Jamestown,  Ind.,  pumping  station  at 165 

Jennings  Oil  Co.,  purchase  of 163 

Jersey  ville,  prospecting  near 16 

Johnson,  H.  H.,  work  of 12 

Jones,  J.  C,  work  of 12 

Jones,  D.  C,  wells  on  farm  of 13 


K 

Kane,  prospecting  near 16 

Kirkwood,   Thomas,   development  of   Kirk- 
wood sand 109 

Kirkwood,  R.  M.,  Xo.  7  well,  record  of 69 

Kirkwood  sand 15 

Anticlinal  dome  in 110 

Correlation  of 109, 182 

Development  of 109 

Drilling  costs 153 

Dips  of HI 

Extent  of 109,  111,  136 

In  Bridgeport  Township 137, 139 

Chester  formations 84 

Dennison  Township 137, 140, 141 

Lawrence  County 109, 135, 138 

Lawrence  Township 137, 139, 141 

Petty  Township 139, 140 

Initial  production  of 109 

Intervals  of 110,  111 

Production  of 135 

Structure  and  thickness  of 110 

Time  required  to  drill  to 153 

Type  locality  of Ho 


440 
Index — Continued. 


PAGE 

LaSalle  anticline 32 

Course  and  extent  of 142, 144 

In,  at  or  near: 

Champaign  Count}- 15 

Clark  County 142 

Sadorus 142 

St.  Francisville 142 

Tuscola 142 

Oil  and  gas  on 143 

Prospective  pools  on 144 

Lawrence  County,  acreage  drawn  on  by  oil 

wells 151 

Bridgeport  sand  of 108 

Buchanan  sand  of 107 

Chester  rocks  of 83 

Cost  of  drilling  in 153 

Development  of 15 

Drilling  time  in 153 

Gas,  depth  of 182 

"  Gas  sand"  in 83, 108 

Gas  wells  in 130 

Geology  of 82, 83, 105, 142 

Importance  of 135, 143, 161 

Kirkwood  sand  of 109 

McClosky  sand  of 112 

Production,  initial 135, 136 

Production  of  sands 105, 135, 163 

Prospective  pools  in 144 

Salt  water  in 140 

Storage  tanks  in 165 

Stratigraphy  of 54, 82 

Structure  of 106, 114, 138, 140, 143 

Tracey  sand  of 84,  111 

Wells  drilled  in 135 

Lawrence  Township,  Buchanan  sand  in  .  .107, 137 

Gas  in 140 

Kirkwood  sand,  type  area  in 137 

McClosky  sand  in 137 

Productions,  initial 135 

Salt  water  in 140, 141 

Structural  relations  in ■. 137 

Wells  in 135 

Lawrenceville,  gas  sold  to 181 

Loading  racks  at 158 

Refinery  at 166 

Lease,  cost  of  operating 161 

Equipment 147, 157 

Use  of 146 

Leasing  of  oil  properties 146, 147, 148 

Lee  County,  gas  in 182 

Lee  Oil  Co.,  purchased  by  Ohio  Oil  Co 163 

Lenses  of  oil  sands 98, 109 

Levels  in  the  oil  field 87 

Lima,  oil  pumped  to 165 

Limestone  as  the  source  of  oil 18 

Lindley,  correlation  of  Kirkwood  sand 109 

Litchfield  oil  and  gas  sands t 12, 13,  29 

Loading  racks,  construction  of 158 

Locke  level,  use  of 94 

Logs  of  cross-section  A-A 115 

B-B 123 

C-C 125 

D-D 130 

Lovington,  axis  near 142 


M 


Macoupin  County,  prospecting  in 15 

Marion  County,  correlation  of  Benoist  sand  . .  109 

"  Gas  sand"  in 182 

Prospecting  in 15 

Storage  tanks  in 165 

Marissa,  prospecting  near 16 

Martin  Township,  dome  in 103 

Marshall,  gas  sold  to 181 

Prospecting  near 16 


PAGE 

Martinsville,  gas  sold  to 181 

Loading  racks  at 158 

Pumping  station  at 164 

Mascoutah,  prospecting  near 16 

McCleave,  S.  G.,  No.  4  well,  record  of 71 

McClosky,  M.,farm 112 

McClosky  oil,  sulphur  in 113 

McClosky  sand 15 

At,  in  or  near:  h 

Bridgeport  Township 139 

Dennison  Township 137, 140 

Lawrence  County 112, 135, 138 

Lawrence  Township 137 

Petty  Township 139 

Ste.  Genevieve  formation 31, 85 

Description  of 85, 113 

Dips  in  Petty  Township 113 

Drilling,  cost  of 153 

Time  of 153 

Extent  of 112 

Origin  of  oil  from 18 

Production  in  Bridgeport  Township 137 

Production,  initial 113, 135 

Salt  water  of 140, 141 

Structural  relations  of 113, 136 

McLeansboro  formation  in  Crawford  County  32, 53 

Mcllroy,  prospecting  by 15 

McOrr  No.  1  well,  record  of 131 

McPherson  No.  3  well,  record  of 67 

No.  4  well,  record  of 68 

Migration  of  oil 18 

Mississippian  rocks,  oil  sands  in 29 

In  Lawrence  County 83 

Missouri-Illinois  Oil  Co.,  shipments  of 166, 169 

Montgomery  County,  prospecting  in 12 

Montpelier,  pumping  station  at 165 

Morgan  county,  gas  wells  in 183 

Muchmore,  pumping  station  at 164 

Muddy  Creek,  pumping  station  at 164 


N 

Nashville ,  prospecting  near 16 

Natural  gas  in  Illinois 181, 183 

Origin  of 18 

New  Hebron,  gas  sold  to * 181 

Newlin,  L.  R.,  No.  21  well,  record  of 38 

Niagara  limestone,  oil  in 13 

Nitroglycerine,  use  of 155, 156, 157 

Northern  Illinois,  geologic  sections  of. 2b 

North  Fork,  pumping  station  at -  164 

North  Fork  Oil  Co.,  purchased  by  Ohio  Oil  Co.  163 
Nutall,  S.  B.,  No.  5  well,  record  of 124 


Oakland,  prospecting  near 14 

Oblong,  gas  sold  to l°i 

Loading  racks  at 1*>° 

O'Donnel  No.  28  well,  record  of °* 

Ohio  Oil  Co.,  acknowledgment  to 12,3d 

Discovery  of  Buchanan  sand  by I07. 

Operations  of 146, 163, 164, 165, 166, 169, 175 

Oil,  accumulation  of 16,  18 

Amount  of  in  Illinois 145 

Circulation  of 18 

Development  of,  in  Illinois 1* 

Diffusion  of j-7 

Geological  work  on 24,95 

Gravitation  of 22 

In  St.  Louis  limestone 31 

Origin  of 16, 18 

Specific  gravity  of 20 

Structural  relation  of 100 

Storage  of 147, 157, 164 

Sulphur  in 21 

Value  of,  in  Illinois 145 


441 
Index — Continued. 


PAGE 

Oil  fields,  description  of 97, 143 

Levels  in 87 

Oil  leases,  specifications  of 148 

Oil  sands,  extent  of 27 

In  Mississippian  rocks 29 

Oil  tanks,  use  of 157 

Oil  wells,  acreage  drawn  on 151 

Elevation  of 94 

Near  Litchfield 13 

Oilfield,  loading  racks  at 158 

Prospecting  near 14 

Oklahoma,  extent  of  petroleum  land 145 

Old  Ripley,  prospecting  near 16 

OIney,  axis  of  Illinois  basin  near 142 

Gas  sold  to 181 

Prospecting  near 10 

Omaha,  prospecting  neajfc. 16 

Ordovician  system 32 

Origin  of  oil  and  gas 16, 17, 18 


P 

Palestine,  gas  sold  to 181 

Parker  &  Edwards,  purchased  by  Ohio  Oil  Co.  163 

Parker  Township,  prospecting  in 12, 14 

Patton,  prospecting  near 16 

Pennsylvania,  extent  of  petroleum  land  in. . .  145 

Pennsylvania  rocks,  extent  of 27 

In  Crawford  County 53 

In  Lawrence  County 82 

Pepple,  A.,  No.  7  well,  record  of 77 

Perkins  No.  16  well,  record  of 122 

No.  17  well 121 

No.  19 75 

No.  22 120 

No.  28 120 

Perry  King  No.  5  well,  Cen.  Refin.  Co.,  record 

of 128 

Petty  No.  1  well,  record  of 116 

No.  3  well,  record  of 117 

Petty  Township,  Bridgeport  sand  in 137 

Buchanan  sand  in 136 

Drift  in 82 

Gas  in 138,139 

"  Gas  sand"  in 108, 110, 136 

Kirkwood  sand  in 110, 136, 139 

McClosky  sand  in 113 

Oil  in 136 

Production,  initial  yield 135, 136 

Salt  water  in 140 

Structural  features  in 113, 136 

Structural  relations  of  oil  and  gas 139 

Tracey  sand  in 139 

Wells  in ; 135 

Phillips,  J.  S.,  prospecting  of 14 

Pike  County,  gas  in 13, 16, 182 

Pinkstaff,  gas  sold  to 181 

Pipe-lines,  use  of,  in  Illinois 148, 167, 169 

Piper  No.  9  well,  record  of 118 

No.  10  well,  record  of 81 

Pleistocene  in  Crawford  County 52 

In  Lawrence  County 82 

Pocahontas,  prospecting  near 16 

Pollution  of  streams  by  waste  oil 160 

Porosity  of  sands 23 

Portable  drilling  rigs,  use  of 153 

Porterville,  gas  sold  to 181 

Pottsville  formation,  description  of 29 

In  Crawford  County 54 

In  Lawrence  County 82 

In  Macoupin  County 15 

Salt  water  in 29, 140 

Structure  of 29 

Studies  of 29 

Thickness  of 29 

Pressure  of  drift  gas 183 

Of  gas  in  Robinson  pool 103 

Of  oil  in  pipe  lines 165 

Princeton,  Ind.,  prices  of  oil  at 169 

—29  Gt 


PAGE 

Prospective  pools  of  Crawford  and  Lawrence 

counties 144 

Pull  rods,  use  of 159 

Pumper,  wages  of 161 

Pumping  equipment 159 

Pumping  stations  in  Illinois 164, 165 

Pure  Oil  Co.,  pipe  lines  of . . 166 


R 

Randolph  County,  correlation  of  sand 109 

Prospecting  in 13 

Rank  of  Illinois  as  gas  state 181 

Rank  of  producing  states 170, 171 

Red  shale,  distribution  of 28, 84, 109 

Rich  view,  prospecting  near 16 

Riddle  Oil  Co.,  purchased  by  Ohio  Oil  Co. ...  163 

Rig,  building  of 152 

Robinson,  gas  sold  to 181 

Loading  racks  at 15$ 

Refinery  at 166 

Robinson  Oil  Co.,  refinery  at  Robinson,  111 166 

Robinson  pool,  accumulation  in 104 

Anticlines  in 99 

Development  of 14 

Extent  of 97, 99, 100, 104 

Gas  in 103 

Production  of 100, 103 

Salt  water  in 103, 104 

Structure  of 99 

Syncline  in 99 

Robinson  sand,  absence  of 98 

Correlation  of 98 

Description  of 97, 98 

Gas  in 99 

Oil  in 100 

Production  of 100 

Thickness  of 98, 100 

Robinson  Township,  prospecting  in 13 

Gas  in 103 

Rock  pressure,  effect  of 20 

Roger  and  Dibble,  shipments  of 166, 169 

Royalty,  payment  of 147 


Sadorus,  anticline  near 142 

St.  Francisville,  anticline  near 142 

Salt  water  in: 

Robinson  pool 104 

Bridgeport  sand 140, 14 1 

Bridgeport  Township 140 

Buchanan  sand 107 

Dennison  Township 141 

Kirkwood  sand 140,141 

Lawrence  County 140 

Lawience  Township 140 

McClosky  sand 140, 141 

Petty  Township 140 

Pottsville  formations 29, 140 

Synclines 103, 104, 140 

Tracey  sand 141 

Salt  water,  siphoning  of 159 

Sandoval,  "  Gas  sand"  near 182 

Oil  prices  at 169 

Prospecting  near 15 

Pumping  station  at 164 

Sands,  correlation  of 95 

Names  of 95 

Porosity  of 23 

Saturation  line  of  sands 143 

Savage,  T.  E.,  work  of 28 

Seed,  H.  K,  No.  1  well,  record  of 132 

No.  2  well,  record  of 131 

No.  7  well,  record  of 61 

Shale  as  the  origin  of  oil 17, 18, 21 

Shallow  sands,  distribution  of 29, 99, 106 

Shiltz,  M.,  No.  7  well,  record  of 33 


442 

Index — Oonohiflod . 


PAGE 

Shipman,  pumping  station  at 164 

Shire,  J.  W.,  farm  of 14 

Shooting  oil  wells 155, 15(3, 157 

Siler,  C.  E.,  No.  4  well,  record  of 41 

Silurian  formations 31 

Smith  No.  24  well,  record  of 130 

Snyder,  W.  H.,  No.  7  well,  record  of 55 

Southern  Illinois,  geological  sections  of 20 

Sparta  oil  field 15 

Sparta  sand,  correlation  of 109 

Specific  gravity,  effect  of 20 

S  pecifications  of  oil  leases 148 

Spudding,  method  of 154 

Ste.  Genevieve  limestone,  description  of.31,  si,  113 

In  Lawrence  County 84 

In  Monroe  County 81 

St.  Louis  limestone,  description  of 85 

Distinguished  from  Ste.  Genevieve 113 

In  Lawrence  County 85 

Oil  in 31 

Standard  rig,  use  of 152, 153 

Statistics,  method  of  compiling 169 

Steel  derrick,  use  of 153 

Stein  farm,  oil  on 15 

Stoltz  No.  13  well,  Bridgeport  Oil  Co.,  record  of  125 

Storage  tanks 166 

Stoy,  gas  sold  to 181 

Loading  racks  at 158 

Pumping  station  at 164, 166 

Tank  farm  at 165 

Stratigraphy,  definition  of 25 

Of  Bridgeport  sand 106 

Of  Chester  rocks 31 

Of  Crawford  County 32, 53, 54 

Of  Illinois 25 

Of  Lawrence  County 32, 54, 82 

Of  Pottsville  formations 54 

Of  Ste.  Genevieve  limestone 31 

Stream  pollution  by  oil 160 

Structure,  definition  of 25 

Of  Buchanan  sand 107 

Crawford  County 99 

"  Gas  sand" 109 

Illinois 32 

Kirkwood  sand 110 

LaSalle  anticline 142 

McClosky  sand 113 

Pottsville  sand 29 

Tracey  sand 112 

Shown  by  cross-sections 12 

Relation 'to  oil,  gas  and  salt  water 100, 103 

Sulphur  in  McClosky  oil 113 

Method  of  removal 159 

Sumner,  gas  sold  to 181 

Prospecting  near 16 

Sumner  quadrangle,  description  of 86, 89, 93 

Sun  Oil  Co.,  shipments  of 166, 169 

Syncline,  definition  of 22 

T 

Terrace  structure 23 

Tanks,  for  storage 147, 158, 165, 166 

Tank-cars  of  Indian  Refining  Co 166 

Theory  of  origin  of  oil 11 

Of  water  saturation 24 

Thomasboro,  prospecting  near 16 

Thompson,  D.  G.,  work  of: 12 

Tidewater  Pipe  Line  Co.,  pipe  lines  of 166, 169 

Tolono,  prospecting  near 15 

Topographic  surveys  of  oil  areas 86 

Townships,  abbreviation  of 96 

Tracey,  pumping  station  at 164 


Tracey,  R.  J.,  farm,  Tracey  sand  on m 

Tracey  Heirs  No.  1  well,  record  of. ,  134 

Tracey  sand .."...     15 

Character  of !!!!!!!!"iil  112 

Development  of '  \\\ 

Drilling,  cost  of 15;} 

Gasin 138  139 

In  Dennison  Township 13s 

Lawrence  County S i,  i  i i,  135, 138 

Petty  Township j;$q 

Oil  from ig 

Structure  of 112 

Type  localities  of 1 1 1 

Transporting  oil 163  ku 

Trenton,  prospecting  near '   16 

Tribune  formation,  description  of .31  83 

In  Lawrence  County  .* 83 

Tubing  for  wells 157 

Tuscola,  course  of  anticline  near 142 

U 

Udden,  Dr.  J.  A.,  work  of 12,  28, 34  53  85 

Ulrich,   description   of  Ste.    Genevieve  lime-' 
stone  by $4 

U.  S.  Geological  Survey,  work  of '.  'sf>,  87 

V 

Vandalia,  prospecting  near \q 

Vincennes,  gas  sold  to '....'.'.  181 

Vincennes  quadrangle,  description  of 86,93  94 

Vanatta  No.  1  well,  record  of ' .  ' 80 

No.  7  well,  record  of ....    7s 

W 

Wapella,  drift  gas  near 183 

Waste-pits,  use  of 159, 160 

Water  saturation  line  of  LaSalle  anticline '  143 

Waterloo,  prospecting  near if, 

Watson,  W.  F.,  shipments  of 169 

Waverly,  prospecting  near 10 

Wayne  County,  basin  in 142 

Well  or  wells: 

Abandoned  in  Illinois 1  si 

Completed  in  Illinois 179 

Drilled  in  Lawrence  County 135 

In  Illinois 12 

Off-setting  of 151 

Well  data,  tables  of 185 

Well  locations 151 

Well  numbers,  system  of 96 

Well  records,  collection  of 94 

Well  samples,  examination  of 34 

Well  sites,  choosing  of 151 

Well  supplies,  cost  of 161 

Westfield,  gas  sold  to 181 

West  Virginia,  extent  of  petroleum  land 145 

White,  David,  study  of  Pottsville 29 

Wild-cat  drilling 152, 162 

Willey  No.  4  well,  record  of . .' 76 

No.  11  well,  record  of 128 

Wilson,  J.  E.,  No.  21  well,  record  of 49 

Wood  No.  13  well,  record  of 79 

Wright,  Douglas,  work  of 12 

Y 

Young  farm ,  prospecting  on U 


